the Creative Commons Attribution 4.0 License.

the Creative Commons Attribution 4.0 License.

# Evidence of the nonstationarity of the terrestrial bow shock from multi-spacecraft observations: methodology, results, and quantitative comparison with particle-in-cell (PIC) simulations

### Christian Mazelle

### Bertrand Lembège

The nonstationarity of the terrestrial bow shock is analyzed in
detail from in situ magnetic field measurements issued from the fluxgate magnetometer (FGM)
experiment of the Cluster mission. Attention is focused on statistical
analysis of quasi-perpendicular supercritical shock crossings. The present
analysis stresses for the first time the importance of a careful and
accurate methodology in the data processing, which can be a source of
confusion and misunderstanding if not treated properly. The analysis performed
using 96 shock front crossings shows evidence of a strong variability of the
microstructures of the shock front (foot and ramp), which are analyzed in
great detail. The main results are that (i) most statistics clearly show that the
ramp thickness is very narrow and can be as low as a few $c/{\mathit{\omega}}_{\mathrm{pe}}$
(electron inertia length); (ii) the width is narrower when the angle
${\mathit{\theta}}_{{B}_{n}}$ (between the shock normal and the upstream magnetic field)
approaches 90^{∘}; (iii) the foot thickness strongly varies, but its
variation has an upper limit provided by theoretical estimates given in
previous studies (e.g., Schwartz et al., 1983; Gosling and Thomsen, 1985;
Gosling and Robson, 1985); and (iv) the presence of foot and overshoot, as shown
in all front profiles, confirms the importance of dissipative effects.
Present results indicate that these features can be signatures of the shock
front self-reformation among a few mechanisms of nonstationarity identified
from numerical simulation and theoretical studies.

A comparison with 2D particle-in-cell (PIC) simulation for a perpendicular supercritical shock (used as reference) has been performed and shows the following: (a) the ramp thickness varies only slightly in time over a large fraction of the reformation cycle and reaches a lower-bound value on the order of a few electron inertial length; (b) in contrast, the foot width strongly varies during a self-reformation cycle but always stays lower than an upper-bound value in agreement with the value given by Woods (1971); and (c) as a consequence, the time variability of the whole shock front is depending on both ramp and foot variations.

Moreover, a detailed comparative analysis shows that many elements of analysis were missing in previous reported studies concerning both (i) the important criteria used in the data selection and (ii) the different and careful steps of the methodology used in the data processing itself. The absence of these precise elements of analysis makes the comparison with the present work difficult; worse, it makes some final results and conclusive statements quite questionable at the present time. At least, looking for a precise estimate of the shock transition thickness presents nowadays a restricted interest, since recent results show that the terrestrial shock is rather nonstationary, and one unique typical spatial scaling of the microstructures of the front (ramp, foot) must be replaced by some “variation ranges” (with lower-bound and upper-bound values) within which the spatial scales of the fine structures can extend.

Collisionless shocks are of important interest in space physics, plasma physics, and astrophysics. These are commonly believed to be important source regions of very energetic particles. The analysis of the shock front fine structures is a key question since it specifies the processes of particles energization that are taking place locally. One major difficulty lies in the fact that different processes take place over different spatial ranges and timescales and may interact with each other.

One can distinguish three main development stages in the front structure studies: first, early attempts to determine shock scale were performed by Holzer et al. (1966) from the magnetic field measurements issued from the Orbiting Geophysical Observatory A (OGO-A) satellite. The technique used at that time was applied to data of EXPLORER 12 (Kaufmann, 1967) and OGO-1 spacecraft (Heppner et al., 1967). Despite some strong assumptions, shock velocity estimates of ∼ 10 km/s were obtained in agreement with some later measurements (e.g., Balikhin et al., 1995). An improved approach has been performed by using two “almost” simultaneous crossings of the shock front by OGO-5 and HEOS-1 (Highly Eccentric Orbit Satellite) spacecraft (at that time we were still before the launch of the ISEE mission (International Sun-Earth Explorer)), which were quite distant from each other (Greenstadt et al., 1975). The shock velocity has been estimated by assuming that the shock surface is planar (no front rippling). This assumption was scrutinized during the shock crossings by Greenstadt et al. (1972, 1975). However, this method cannot apply to a large number of shock crossings, because the probability that two different spacecraft remain close to each other and cross the same bow shock almost simultaneously is quite low. However, both techniques produce values of the laminar shock thickness (i.e., identified later as subcritical shocks), in agreement with later measurements by ISEE spacecraft (Russell et al., 1982).

Second, the studies on dual-spacecraft missions such as ISEE-1 and ISEE-2 and later AMPTE (Active Magnetospheric Particle Tracer Explorer) considerably improved our knowledge of shock structures and classification (e.g., quasi-perpendicular (parallel) and subcritical (supercritical) shocks). At that time, even though significant efforts had been focused on quantifying the thickness of subcritical shock fronts with different methods, a major difficulty still persisted. According to different theories, the shock thickness seems to be similar (Balikhin et al., 1995). The large number of reliable shock velocity and thickness estimates from dual-spacecraft studies, with small inter-spacecraft separation, allowed researchers to overcome this difficulty (Russell et al., 1982). However, statistics from multi-spacecraft studies have shown that subcritical shocks are relatively rare; i.e., the terrestrial bow shock is typically supercritical (Balikhin et al., 1995). Profiles of supercritical shocks are more complex than for subcritical ones. Other methods have been proposed to estimate the widths of the microstructures (ramp, foot, overshoot) identified within the front of a supercritical shock. ISEE-1 and ISEE-2 observations have strongly stimulated the analysis of their spatial thickness (Livesey et al., 1982, 1984; Gosling and Thomsen, 1985; Mellott and Livesey, 1987; Scudder et al., 1986). However, at that time, the vision of most studies was mainly based on a stationary terrestrial bow shock; the scaling was referring the thickness of the whole shock front (and not its microstructures), and this thickness has been expressed in terms of the ion inertial length scale.

Third, an improved approach has been supported by the quadri-satellite Cluster mission, which not only allowed us to analyze in great detail the fine structures within the shock front itself but also clearly showed that the terrestrial bow shock can be strongly nonstationary (Horbury et al., 2001, 2002; Walker et al., 1999; Moullard et al., 2006; Mazelle et al., 2010a; Lobzin et al., 2007, 2008; Lefebvre et al., 2009; Meziane et al., 2014, 2015). More generally, the nonstationarity of quasi-perpendicular shocks in a supercritical regime has also been shown in plasma laboratory experiments several decades ago (Morse et al., 1972), and it was largely analyzed in numerical simulations (Biskamp and Welter, 1972; Forslund et al., 1984; Lembège and Dawson, 1987; Winske and Quest, 1988; Lembège and Savoini, 1992; Lembège et al., 2008, 2009; Nishimura et al., 2003; Scholer and Matsukiyo, 2004; Chapman et al., 2005). Particle-in-cell (PIC) and hybrid simulations clearly show different processes as sources of the shock front nonstationarity, which are summarized as follows (Lembège et al., 2004):

- a.
The first is the self-reformation driven by the accumulation of reflected ions at a foot distance from the ramp. During their coherent gyromotion, the reflected ions accumulate at roughly the same location and build up a foot whose amplitude largely increases in time until its upstream edge suffers an important steepening and becomes a new ramp. New incoming ions are reflected at this new ramp, and the same process continues cyclically. This process has shown to be quite robust since it was shown originally in 1D PIC simulations (Biskamp and Welter, 1972; Lembège and Dawson, 1987; Lembège and Savoini, 1992; Hada et al., 2003; Scholer et al., 2003; Scholer and Matsukiyo, 2004), later in 2D (Lembège and Savoini, 1992), in 1D/2D hybrid (Hellinger et al., 2002, 2007), and in 3D PIC simulations (Shinohara et al., 2011). The self-reformation persists for oblique propagation and disappears (i) when the oblique direction of the shock front normal is below a critical angle for which the density of newly reflected ions is too weak to feed the ions accumulation (Lembège and Savoini, 1992) and (ii) for shocks with higher

*β*_{i}(the ratio between thermal ion pressure and magnetic pressure) (see Sect. 5.1), as shown by Schmitz et al. (2002) and Hada et al. (2003), or equivalently as the ratio ${v}_{\mathrm{sh}}/{v}_{\mathrm{thi}}$ is relatively weak (a few units) (Scholer et al., 2003), where*v*_{sh}is the shock velocity in the solar wind rest frame, and*v*_{thi}is the upstream ion thermal velocity (solar wind protons). As will be discussed in Sect. 5.1, this self-reformation process persists well even in the presence of microinstabilities developing within the front for perpendicular shocks (Muschietti and Lembège, 2006). - b.
A similar self-reformation is also observed in 1D PIC simulation of an obliquely propagating shock (in a configuration not exactly perpendicular) but has a different origin since it is mainly driven by a microinstability (MTSI or modified two-stream instability) excited by the relative drift between incoming electrons and incoming ions within the foot region. This instability develops quickly enough to thermalize the ions and generates a pressure increase which contributes to the buildup of a new ramp (Matsukyio and Scholer, 2003; Scholer and Matsukiyo, 2004). In addition to low

*β*_{i}, high and realistic mass ratio and a slightly oblique propagation are necessary conditions (small but finite component of wave vector parallel to the ambient magnetic field) for the MTSI to be excited. - c.
The so-called “gradient catastrophe” process (Krasnoselskikh et al., 2002), which results only from an imbalance between nonlinear and dispersive effects (Galeev et al., 1999), is expected as the Alfvén Mach number,

*M*_{A}, is above a critical threshold (or equivalently the shock front propagation angle is below a critical value). When this condition is satisfied, large-amplitude nonlinear whistler waves are emitted from the ramp and are responsible for the front nonstationarity. This process also requires a slightly oblique propagation necessary for the emission of these nonlinear whistler waves. However, this theoretical process has very strong constraints as it is based on the 1D model only and excludes any dissipative effect. Indeed, reflected ions (which play a key role in the supercritical Mach regime) are neglected, and their impact on the shock dynamics is totally absent. - d.
The last is the emission of large-amplitude whistler waves within the front, which propagate obliquely both to the shock normal direction and to the static magnetic field; this mechanism has initially been shown for a perpendicular shock (Hellinger et al., 2007; Lembège et al., 2009) and later for a quasi-perpendicular shock by Yuan et al. (2009). It is basically a 2D mechanism, which has been retrieved both in 2D-hybrid and 2D-PIC simulations, and has been observed in 3D PIC simulation (Shinohara et al., 2011). One expects that the presence of these waves within the front enlarges the width of the ramp (since these propagate almost at the same velocity as the shock front), but no detailed measurement has been reported yet. One proposed mechanism could be the ion Weibel instability triggered by the reflected gyrating ions (Burgess et al., 2016). Up to now, the mechanism responsible for this wave emission has not been clearly identified yet.

This paper represents an extensive and more detailed analysis of previous studies (Mazelle et al., 2007, 2008a, b, 2010a, b, 2011, 2012). Its aim is motivated by the following questions. (i) What important precautions are necessary when measuring carefully the spatial widths of the fine structures (foot and ramp) of the shock front from experimental data? (ii) What are the sources of confusion or misunderstanding when comparing the present results (based on statistics of shock crossings) to interpretations of experimental data made in previous analyses mainly based on one or a few shock crossings only? (iii) Among the different mechanisms proposed as sources of the shock front nonstationarity, is it possible to extract some features from the shock front microstructures (observed in experimental data), allowing us to clearly identify the dominant nonstationary processes?

The paper is organized as follows. Section 2 presents the motivation, data selection, and methodology. A detailed analysis of individual shock crossings is presented in Sect. 3. The results of a statistical analysis and the comparison with PIC numerical simulation results are reported in Sect. 4. Section 5 is devoted to the comparison with previous studies (both experimental and numerical), and Sect. 6 draws some conclusions.

## 2.1 Experimental data

The constraint on time resolution necessitates the sole use of the magnetic field data for the present detailed analysis. Particle data will be used only to provide the necessary “contextual” plasma parameters, since their time resolution is commonly much lower than the magnetic field data. The latter are provided by the fluxgate magnetometer (FGM) (Balogh et al., 2001). Since the thicknesses of the shock front microstructures must be determined accurately, the use of the best time resolution is vital, i.e., 22 to 66 Hz depending on the available telemetry. But, lower time-resolution data (5 and 1 Hz) are also used for comparison and to confirm the temporal extension of shock front microstructures (mainly the ramp and the magnetic foot; the overshoot or undershoot is not analyzed in detail here) when the level of microturbulence is relatively high. This is also very important for validating the determination of the shock normal vector (see Sect. 2.2).

Using the appropriate data from both Cluster and ACE (Advanced Composition Explorer) satellites, the major
shock parameters have been derived: the alfvénic and magnetosonic Mach
numbers *M*_{A} and *M*_{MS}, the angle ${\mathit{\theta}}_{{B}_{n}}$ between the upstream
interplanetary magnetic field and the local shock normal, and the ion
*β*_{i}. We use herein Cluster particle data from the Cluster Ion
Spectrometry (CIS) experiment which is extensively described in Rème et
al. (2001). It consists of two sensors: (i) a hot-ion analyzer (HIA)
measuring particles within the energy range 0.005–26 keV and (ii) a
time-of-flight mass spectrometer (CODIF), combining a top-hat analyzer with
a time-of-flight section to measure the major species H^{+}, He^{+}, He^{2+},
and O^{+} covering an energy range extending from 0.02 to 38 keV/e (where e is the unit electrical charge). Both
instruments allow us to measure full 3D distributions with a typical angular
resolution of 22.5^{∘} × 22.5^{∘} within one
satellite spin period (4 s). Two operational modes are possible: in
“normal” telemetry modes, one distribution is transmitted every two or
three spins (depending on the time of measurements), whereas in “burst”
telemetry modes the distribution is transmitted at every single spin. With
the instrumental characteristics mentioned above, both the solar wind plasma
and the energetic particles are detected. The measurements with the HIA are performed with high geometry factor (HIA-G), suitable for
upstream ion measurements, and with low geometry factor (HIA-g),
suitable for the solar wind plasma measurements, which use specific narrower
angular bins (5.6^{∘} × 5.6^{∘}). We are primarily interested
in the moments of the velocity distribution obtained from both “solar wind”
modes and “magnetospheric” modes of the HIA instrument. The best
determination of the upstream solar wind parameters (density, velocity, and
temperature) is obtained for a “solar wind” mode where HIA-g data are
available. For a magnetospheric mode, the solar wind velocity is still
correctly determined though less accurately than in a solar wind mode;
however, the density is often underestimated, and the temperature is
overestimated by a large factor when compared to other data sets (for
details, see Rème et al., 2001). The density underestimate is due to a
saturation effect for the solar wind beam, while the temperature overestimate
is due to the use of wide angular bins of the high-G part of the HIA
instrument. In this case, we use ACE satellite data considering the proper
time shift between ACE and the Cluster constellation.

Figure 1 displays a typical example of a quasi-perpendicular shock crossed by the Cluster spacecrafts. The top panels show the profiles of the magnetic field magnitude measured by FGM at the spin time resolution (4 s average). The profiles seem very similar at first glance and do not allow for any precise determination. In contrast, the bottom panels show the same shock crossing with high time-resolution data. Many differences are clearly revealed, which illustrate the necessity to use the best possible time resolution. The methodology used here needs a relatively short separation distance between all four satellites in term of ion inertial length. This was the case only during the spring seasons of 2001 and 2002 for which all the inter-distances lied between 100 and 600 km typically, which is not the case for more recent satellite configurations (Escoubet et al., 2015). Moreover, the Earth's bow shock is often crossed many times by the four satellites in this configuration as the quartet remains nearby the shock front itself while the shock is globally moving inward and outward.

## 2.2 Methodology

We detail for the first time a new methodology to carefully analyze
experimental data for the study of supercritical quasi-perpendicular
shocks. The step-by-step analysis method we have developed is illustrated in
Fig. 2 and is conceptually straightforward. First, for each satellite, the
temporal extension of each microstructure of the shock front is determined
in the time series of the magnetic field. For each of them, beginning and
end times are first estimated by visual inspection. For many previous
studies in the literature, the process usually stops at this level, leaving
the possibility of strong bias. Here, this first step is made only to
initialize later automatic algorithms which will be used eventually to
determine spatial error bars (both for the outer and inner edge of each
microstructure). For each beginning or end time of a microstructure, we
get a first estimate of an error bar on it by defining two associated times:
one time (e.g., *t*_{a}) when the spacecraft has already likely entered the
shock front or left the previously estimated microstructure and a second time
(e.g., *t*_{b}) when the spacecraft is inside the present
microstructure for sure. The order of these two times obviously depends
on whether there is an inbound or outbound bow shock crossing. This may appear
arbitrary and occasionally difficult to estimate, but experience shows
that the risk to miss the real beginning and end times inside the defined
interval is very low. Different stages of the present methodology are
summarized in Fig. 2 and are detailed below.

### 2.2.1 Determination of asymptotic upstream and downstream parameters

The determination of upstream parameters entails a steady asymptotic
upstream interplanetary magnetic field (IMF) *B*_{0} associated with each shock crossing by the
four spacecraft. For highly perpendicular shocks, however, it is often
possible to define an unperturbed upstream field on a timescale of around a
few minutes. For each satellite, we must define an upstream time interval
displaying a magnetic field quite steady both in components and magnitude.
For each spacecraft $s/{c}_{i}$, where $s/{c}_{i}$ represents for spacecraft *i* among the Cluster quartet
(where *i*=1 to 4), an average upstream field *B*_{0i} is computed. Its magnitude is shown in the
lower horizontal green line in Fig. 3a for one example of a single
spacecraft shock crossing. Again, an initial estimated time interval is
obtained from the visual inspection of the time series. The time duration
cannot be too long since the usual stability timescale of the IMF due to
the intrinsic solar wind variability (turbulence and directional
discontinuities) is rarely more than a few tens of minutes (e.g., Burlaga, 1971), which we can take as an upper limit Δ*t*_{u}. In order to be
physically reliable, Δ*t*_{u} cannot be too short. One reasonable
lower limit Δ*t*_{l} is the time interval during which a solar wind
parcel travels a distance of one ion inertial length (about 100 km usually)
that is about 1 min typically, considering the mean spacecraft
velocities are all unchanged within a reasonable range. In this purpose, the
six relative angles *θ*_{ij} measured between upstream fields
*B*_{0i} and *B*_{0j} for $s/{c}_{i}$ and $s/{c}_{j}$ with ($i,j=\mathrm{1}$ to 4)
are computed. The upstream vector *B*_{0i} measured by satellite *i* must be as close as possible
to the vector *B*_{0j} measured by another
satellite *j*. If all angles *θ*_{ij} are less than 5^{∘} (arbitrary value chosen herein from empirical considerations), then the
procedure is pursued; otherwise, the upstream time intervals (where
these *θ*_{ij} values are calculated) are
automatically modified by slightly shifting and reducing them until the
above constraint on *θ*_{ij} is satisfied. The shock event is
rejected from the present analysis when the adjustment fails or is not
satisfactory.

When possible, the use of a larger time interval improves the statistics.
Using the initial estimate of Δ*t* and constraining it to be between
Δ*t*_{l} and Δ*t*_{u}, the best upstream interval
corresponds to the lowest values of the standard deviations *σ* for
both the magnitude and components of the field. Although this can be easily
verified by visual inspection, it allows us to ensure the absence of any solar
wind disturbance. The following step deals with the determination of a
unique unperturbed ambient IMF *B*_{0} for
every shock crossing by the four-spacecraft constellation. First, it is
necessary to compare the individual upstream fields *B*_{0i}. This determination of *B*_{0} is of crucial importance for the present study
since it impacts both the value of the shock Alfvén Mach number through the
field magnitude used and the determination of the angle ${\mathit{\theta}}_{B{n}_{\mathrm{0}}}$
between *B*_{0} and the global shock normal
*n*_{0}. This is obviously the first possible
source of error in the determination of both the upstream Alfvén velocity,
the Alfvén and magnetosonic Mach numbers, and the angle ${\mathit{\theta}}_{B{n}_{\mathrm{0}}}$.

### 2.2.2 Determination of initial internal and external time limits of the foot

For each satellite, the standard deviations, *σ*, obtained above for the
magnetic field components and magnitude allow for the determination of the time
when the spacecraft penetrates inside the magnetic foot. We determine, for
each component and magnitude, the time when it is above a 3*σ*
threshold level and close to the initially estimated time of the entry into
the foot obtained by visual inspection (*t*_{a} dashed blue line in Fig. 3a). Then, we select the “external” limit of this entry (*t*_{1} in Fig. 3a) among these four times as the closest to the external estimate
*t*_{a}, and we select the “internal limit” (*t*_{2} in Fig. 3a) as the closest to the
internal estimate *t*_{b} (dashed blue lines in Fig. 3a). The derived times,
*t*_{1} and *t*_{2}, then define the error bar of the foot entry in the time
domain. For the present case, the visual estimate *t*_{b} nearly coincides
with the time *t*_{2} automatically determined. Moreover, the possible
presence of solar wind or foreshock transients as well as a detached whistler
wave packet must be avoided. The last case occurs quite often even in the nearly
perpendicular configuration and can easily lead to a wrong determination.
Also, solar wind transients are always possible, while foreshock transients
may only be an issue for a more “oblique” configuration which is not addressed
in the present study. Nevertheless, it is necessary to make a cautious post-visual inspection.

### 2.2.3 Determination of initial internal and external time limits of the ramp

Similarly, the initial estimated times of the other microstructures are
labeled with letters, and the final times determined from the present
methodology are labeled with numbers. The times *t*_{c} and *t*_{d} are the
initial “visual” estimates for the exit from the foot and entry into the ramp,
respectively. They will be only used for initializing the automated
algorithm described below. A major caveat in many previous attempts to
compute the ramp thickness in the literature is to include in the ramp the
part of the magnetic field profile up to the maximum of the first overshoot.
To avoid this and to define at least the first overshoot well, we need to
determine a downstream (asymptotic) level which would be required, for
instance, for checking the Rankine–Hugoniot conditions. For that purpose, it
is necessary to define a downstream interval in the magnetosheath far enough
from the consecutive overshoots or undershoots displaying a quasi-steady
magnetic field. This choice is highly important and not always
straightforward in the case of very close consecutive crossings (multiple
crossings) where only an average over the region of the sequence of
overshoots or undershoots will be estimated. When a “clean” time interval
downstream from this overshoot or undershoot interval is available, the
average values obtained for *B* magnitude and components can be compared to
the values inside the overshoot or undershoot interval. If these values are
in good agreement, the downstream interval is appropriate for the
determination of the asymptotic value. It is then used to give an initial
estimate (*t*_{e}, *t*_{f}) of the final time interval (*t*_{5}, *t*_{6}) for the exit
from the ramp or entry into the overshoot by using ±5 % of the computed
asymptotic value (which is arbitrary but appears to be a good empirical
compromise). It should be mentioned that a 1*σ* level can also be
determined here, but it will usually be large in this region (local
microturbulence in the magnetosheath) and not appropriate for the present
purpose. The two times (*t*_{e}, *t*_{f}) are again only used for initializing
the next automated step.

### 2.2.4 Determination of final internal and external time limits of the ramp with the automatic algorithm

From the initial time estimates (*t*_{c}, *t*_{d}) and (*t*_{e}, *t*_{f}), the
determination of the final times for the entry into and exit from the ramp,
(*t*_{3}, *t*_{4}) and (*t*_{5}, *t*_{6}), respectively, is made with an
automatic algorithm. In order to characterize a steep gradient, we perform a
linear fit of the data points between *t*_{c} and *t*_{f}. The time range for
the regression can vary on both sides. The process is initialized by the
largest possible time interval with *t*_{3}=*t*_{c} and *t*_{6}=*t*_{f}.
Then, the entry time can vary between *t*_{c} and *t*_{d}, while the exit time can vary between *t*_{e} and *t*_{f}. The choice of a linear fit mainly
excludes any “pollution” of the ramp region by a part of the extended foot
(around the upstream edge of ramp) and by downstream fluctuations around the
overshoot (around the downstream edge of the ramp). The resulting time
interval is associated with the best linear regression coefficient, and the
bounding times (*t*_{c} and *t*_{f}) explored during the automatic procedure
are kept to estimate the error bars. In other words, we impose *t*_{3}=*t*_{c} and *t*_{6}=*t*_{f}. The automatic procedure only defines
*t*_{4} and *t*_{5} (internal limits of the ramp). Then, the crossing of the
downstream asymptotic value closer to the first estimate defines the exit
from the overshoot (nearly equivalent to the middle of the gradient between
the first overshoot and the first undershoot, not shown in detail here). The
times *t*_{7} and *t*_{8} for the exit from the first overshoot are defined in
the same way as the entry (Fig. 3a). The time *t*_{g} shown by a vertical
dashed blue line is – as for the other microstructures – simply the initial
rough “visual” estimate and is just shown for reference for a later visual
check.

For every shock crossing by the Cluster quartet, we make the same
procedure for each satellite. The satellite that is associated with the
steeper ramp from this analysis is used to arbitrarily define what is called
the “reference satellite” for a shock crossing event. Then, we determine the
middle time *t*_{ramp,i} of the ramp crossing time interval for each
individual satellite *i* and the “reference time” for a shock crossing is
simply this middle time *t*_{ref} for the arbitrarily chosen reference
satellite. Next, we determine the shock velocity and normal from the four
different middle times *t*_{ramp,i} and the four spacecraft
positions in the GSE (Geocentric Solar Ecliptic ) frame by using the classical “timing method” (e.g.,
Schwartz, 1998; Horbury et al., 2001, 2002). This method works if the
separation between the spacecraft is not too large (otherwise the hypothesis
of a planar structure breaks down) and provided that the four spacecraft are
not coplanar (otherwise the method fails) and that the shape of the
tetrahedron is not very elongated (which is not the case for the present
study). This method provides a global normal vector *n*_{0} valid only at the length scale of the spacecraft
tetrahedron (i.e., the largest inter-distance between two satellites) and at
the temporal scale defined by the time interval between the first crossing
and the last crossing among the four satellites. The error bars for the
entry or exit times are used to determine an error bar for the normal vector. It
must be mentioned that each local normal vector *n*_{i}
for the crossing by $s/{c}_{i}$ can differ from the global *n*_{0} because of the small-scale turbulence of the
front (shock front ripples) but cannot be determined experimentally as
reliably as *n*_{0} by any classical
single-spacecraft method. Moreover, as will be discussed later, we intend
here to compare the values determined experimentally with simulation
results for which the normal vector *n*_{0} and thus the ${\mathit{\theta}}_{B{n}_{\mathrm{0}}}$ angle are
globally defined for a shock front both averaged spatially perpendicular
to the normal and in time (see Sect. 4.4). This will also
conversely justify the averaging along the shock front made in the
simulations (that will be described in Sect. 4.4). The local effect due to
the variation of the local normal direction *n*_{i} with
respect to *B*_{0} (local curvature effect
due to the shock rippling at a lower scale) is not analyzed in the present
work.

### 2.2.5 Transition criteria from “temporal” to “spatial” profiles of a parameter

For all the shock front microstructures, the above analysis gives an
“apparent” temporal extension along each satellite path and allows us to
compare them between the four satellites. In every individual spacecraft
frame, we compute an individual shock velocity vector. Since the spacecraft
velocities in the Earth frame are typically around a few kilometers per second (km/s) as also found
for many slowly moving shocks in the same frame, it is essential to also
take these small spacecraft velocities into account. The major aim of the
present analysis is to reconstruct a local spatial profile along the
global shock normal *n*_{0} as shown in
Fig. 3b. For this purpose, the angle between each spacecraft *i*
trajectory and *n*_{0} has been used. Then,
it is possible to measure the local physical thicknesses along *n*_{0} of the microstructures of the shock front and
compare them between the different satellites. It must be mentioned that the
shock velocity determined by the four-spacecraft timing method here is an
averaged velocity within the time interval separating the first and the last
shock crossings. Then, it is supposed to be constant during this time
interval and homogeneous over the spatial scale of the tetrahedron. One
cannot preclude that the shock velocity can vary inside the considered time
interval and that the shock motion is subject to some acceleration inward
and/or outward. However, this possible effect can be assumed as weak if the
temporal profiles of the shock crossing are quite similar in time series
taken at low temporal resolution (such as in Fig. 1a). In contrast, when a
sudden shock front acceleration or deceleration (due to a solar wind
fluctuation) occurs between the crossings by two satellites, there is a
clear signature in the time series (see in Fig. 4, derived from Fig. 1 in
Horbury et al., 2002). Figure 4b and c are typical cases of observations which
are eliminated from our present analysis. We use the same shock velocity in
the Earth's frame for the four crossings to derive the spatial widths along the
global normal *n*_{0} for any case like in
Fig. 4a.

Then, we can compare the obtained thicknesses of the shock microstructures with physical length values predicted either by theory or from numerical simulation results. It must be mentioned that using only time series can lead to wrong comparative classification of the observed crossings. A large angle between the spacecraft velocity vector and the shock front normal can produce a long crossing duration for a real very small physical thickness and will also produce a small shock speed. In summary, a particular precaution is necessary to avoid conclusions deduced exclusively from the temporal profiles, especially in the selection process which is often based solely on the steepness of the temporal gradient in the literature.

In order to have a qualitative check of the determination of the global
normal *n*_{0}, the time series of the
component *B*_{n} of the instantaneous magnetic field along this normal is
systematically examined. First, this normal component is supposed to be
conserved on both sides of the shock front. Second, for a nearly
perpendicular shock, this component is expected to vanish (exactly zero for
90^{∘} shock) upstream from the shock front and inside the ramp,
since the vector of the magnetic field is supposed to be strictly along the
shock front. Figure 5 displays the temporal evolution of *B*_{n} for a shock
front crossing on 31 March 2001 around 17:38 UT for one of the four satellites
(magenta lower curve) in comparison with the total magnitude *B* (black upper
curve). For this shock, the ${\mathit{\theta}}_{{B}_{n}}$ angle is about 86^{∘}.
If one takes into account the fluctuations observed in and around the ramp,
the conservation in the front is well respected, and the upstream value is
also very low as expected for a nearly perpendicular case. The downstream
evolution in the overshoot is also consistent with expected oscillations
around the average downstream value (e.g., Kennel et al., 1985).

## 3.1 One typical case

A typical example of the spatial profiles is shown in Fig. 6. It is
obtained for one supercritical quasi-perpendicular shock crossing by Cluster
on 31 March 2001 at 17:38 UT (${\mathit{\theta}}_{{B}_{n}}=\mathrm{86}\pm \mathrm{2}$^{∘},
*M*_{A}=4.1, *β*_{i}=0.05) when the $s/c$ separation was about a few
ion inertial lengths $c/{\mathit{\omega}}_{\mathrm{pi}}$ (herein $c/{\mathit{\omega}}_{\mathrm{pi}}$ = 80–120 km,
typically). The profiles are ordered by the sequence of crossings starting
from satellites C4 to C3 (top to bottom in Fig. 6a and b). The relative
locations of the four $s/c$ defined at the reference time given by satellite
C4 (see Sect. 2.2) are represented in the plane containing both the
*X*_{GSE} direction and the normal *n*_{0}
(Fig. 6c) and in the plane perpendicular to the normal *n*_{0} (Fig. 6d).

In a first approach, the differences between the $\mathrm{4}s/c$ spatial profiles in Fig. 6b are quite obvious, particularly for the magnetic foot and the overshoot widths; however, these are less evident for the ramp. We emphasize that all upstream conditions remain unchanged for all four satellites. As a consequence, this shows the strong variability of the quasi-perpendicular shock front itself. We stress that the ramp widths can be very narrow and can reach values as low as a few electron inertial lengths with the thinnest one reaching $\mathrm{5}c/{\mathit{\omega}}_{\mathrm{pe}}$ for satellite C4. This result strongly disagrees with the typical scale length of the ramp commonly considered around $c/{\mathit{\omega}}_{\mathrm{pi}}$ (e.g., Russell and Greenstadt, 1979; Scudder et al., 1986; Bale et al., 2005), although it is in very good agreement with some “exceptional” ISEE results (Newbury and Russell, 1996; Newbury et al., 1998) as well as theoretical studies predicting the existence of small scales in quasi-perpendicular shocks as a signature of the front nonstationarity or results issued from PIC numerical simulations (Lembège and Dawson, 1987; Lembège and Savoini, 1992; Lembège et al., 1999, 2013a, b; Scholer et al., 2003; Marcowith et al., 2016, and references therein).

This nonstationarity can also be shown in the content of Fig. 6. The
C3 and C4 satellite locations are almost aligned with the direction *n*_{0}
(Fig. 6c) and are close to each other (over a distance of less than
$c/{\mathit{\omega}}_{\mathrm{pi}}$) in the plane perpendicular to *n*_{0} (Fig. 6d). If the shock
front was stationary, after propagating from C4 to C3, the profiles are
expected to be nearly identical, but they appear significantly different. For
instance, the spatial ramp thickness for C3 is about twice the one for C4,
and the shape and thickness of the overshoot are also very different.
Moreover, C2 and C1 locations are not far enough to be along the *n*_{0} direction (Fig. 6c), but they depart
from each other in the perpendicular plane to *n*_{0} (i.e., along the shock front) by
several $c/{\mathit{\omega}}_{\mathrm{pi}}$ (Fig. 6d). The differences mentioned here can be
related to the shock front nonuniformity due to its rippling;
the impact of this rippling on the front variations will be analyzed in a
future work.

## 3.2 Impact of the shock velocity

A careful determination of the shock velocity is necessary in order to
discuss the physical spatial thicknesses of the shock front microstructures.
This also means that it is not possible to consider only time series to
discuss the relative properties of different shock crossings. Moreover, as
already stated previously, the time resolution of the data needs to be
considered before any conclusion. This is illustrated in Fig. 7. The left
part shows the time series of the magnetic field components and magnitude
for two shock front crossings and for two different time resolutions each
(panels a1 and b1): the highest available resolution (15 or 60 ms depending
on the mode) and the spin resolution of 4 s. These two shocks have been
chosen as they are characterized with similar parameters ${\mathit{\theta}}_{{B}_{n}}$,
*M*_{A}, and *β*_{i}. The first shock a (panel a1) is a slow-moving shock
with a velocity of about 11 km/s, while shock b (panel b1) is a fast-moving
shock with a velocity of about 78 km/s. When considering the lowest time
resolution (averaged data on 4 s), the two profiles in the upper plots of
panels a1 and b1 appear very similar. If only data with this time
resolution were considered, one should have concluded at first glance that
the two shock crossings are very similar and display very similar properties
with relatively smooth time gradients of a similar shape. But, the highest
time resolution on the lower panels reveals
the large difference between shock profiles when changing the data sampling:
shock b appears steeper than shock a. Moreover, for shock a, the
gradient remains nearly unchanged with only superimposed higher-frequency
fluctuations which are not observed upstream from the sharp front displayed
by shock b. The full shock properties are revealed only if the spatial
profiles, as shown on panels a2 and b2, are considered. The general
shapes of the shock front microstructures are very similar for the two
shocks, but the steeper spatial ramp is obtained for shock a, while shock
b displays a ramp spatial thickness more than twice that of shock a
(right-hand panels a2 and b2, respectively). Moreover, it also reveals
that the structure of the shock is better sampled up to much higher
frequencies for a slow shock velocity. In the spacecraft frame, any
instrument like the magnetometer uses a constant sampling frequency and thus
obviously measures much fewer measurement points inside any shock front
microstructure when this one is propagating faster. This example illustrates
quite well the advantages of the methodology developed in the present study
to correctly address the spatial scales of a shock front and the careful
precaution to keep in mind when analyzing only the temporal shock profiles.

## 4.1 Selection criteria

An analysis similar to the one described in Sect. 3 has been performed for a
list of shocks after a severe selection procedure. Several criteria have
been used: (i) limitation to shocks normal direction ${\mathit{\theta}}_{{B}_{n}}$
approaching 90^{∘} as much as possible (more than 75^{∘}) in
order to avoid more complex mechanisms which take place at oblique shocks
(Lembège and Savoini, 1992; Lembège et al., 2004; Marcowith et al.,
2016), (ii) existence of well-defined upstream and downstream ranges for
each of the $\mathrm{4}s/c$, (iii) stability of the upstream averaged magnetic field
from one $s/c$ to another, (iv) validity of the normal determination by
checking the weak variability of the normal field component *B*_{n} around
the ramp and low value of ${B}_{n}/\left|\mathit{B}\right|$ upstream for ${\mathit{\theta}}_{{B}_{n}}$
close to 90^{∘}, (v) availability of all data necessary to compute
the shock parameters, and (vi) a maximum spacecraft separation distance
limited to a few $c/{\mathit{\omega}}_{\mathrm{pi}}$ between the four spacecraft in order to
consider the crossing of a same “individual” shock front by all Cluster
spacecraft. From an initial ensemble of 455 shock crossings (including
essentially data for 2001 and 2002 for which spacecraft separation distances
are all small enough), only 24 shock events have been selected after the
validation of the aforementioned criteria. This implies a detailed analysis
of 96 individual shock crossings. Figure 8 displays the distributions of
four main parameters ${\mathit{\theta}}_{{B}_{n}}$, *M*_{A}, *β*_{i}, and
${v}_{\mathrm{sh}}/{v}_{\mathrm{thi}}$ (see Sect. 1). For the selected shock crossings, the
${\mathit{\theta}}_{{B}_{n}}$ values extend from almost 90 to 75^{∘} but mostly above 84^{∘} (80 %), the *M*_{A} values of the resulting
shocks are equally distributed from 2 to 6.5, the ratio ${v}_{\mathrm{sh}}/{v}_{\mathrm{thi}}$
between 2 and 30 with a peak within the range 12–24, and *β*_{i}
extends from very low values to 0.6 but with 67 % of values less than 0.1.

## 4.2 Ramp thickness

The obtained ramp thickness distribution shown in Fig. 9a appears
Gaussian, indicating that most of the shocks are associated with a narrow
ramp. Interestingly, the distribution reveals a cutoff mark at $c/{\mathit{\omega}}_{\mathrm{pi}}$. Figure 9b displays the thinnest ramp found among each quartet of
crossings for each individual shock versus ${\mathit{\theta}}_{{B}_{n}}$. No simple
relation emerges. However, many observed thinnest ramps have a width of less
than $\mathrm{5}c/{\mathit{\omega}}_{\mathrm{pe}}$, and the magnetic ramps thickness tends to reach low
values when approaching 90^{∘}. Figure 9c and d display scatter
plots of all ramp thicknesses versus ${\mathit{\theta}}_{{B}_{n}}$ and *M*_{A},
respectively; for clarity, individual error bars are not reported on the
figure.

Although Fig. 9c shows no clear dependence of the ramp width with
${\mathit{\theta}}_{{B}_{n}}$, it indicates that the narrowest ramps are
associated with nearly perpendicular geometries as pointed out by the red
arrow. Figure 9c also shows that the ramp thickness variation is not solely
controlled by the shock geometry. It can vary a lot for a single value of
${\mathit{\theta}}_{{B}_{n}}$ except maybe when close to 90^{∘}. Moreover, the ramp
thickness obtained from the analysis of a same crossing with each single $s/c$
appears inconsistent (up to a factor 7) although the upstream conditions
remain similar. This illustrates quite well the signature of an intrinsic
shock front nonstationarity. Figure 9d does not reveal any simple relation
of the shock ramp thickness with *M*_{A}. It may only illustrate that the
maximum observed thickness reduces as the Mach number increases, although
the scatter plot and the statistics do not allow us to make any other
conclusive result.

The statistics confirm the important result, shown in the individual case study of Sect. 3, that the magnetic field ramp of a supercritical quasi-perpendicular shock often reaches a few $c/{\mathit{\omega}}_{\mathrm{pe}}$. The time variability of scales observed for the same upstream conditions is also consistent with a signature of the front nonstationarity due to the self-reformation fed by the accumulation of reflected ions in agreement with PIC and hybrid simulation results (Lembège and Dawson, 1987; Biskamp et Welter, 1972; Lembège et al., 2004; Lembège and Savoini, 1992; Hellinger et al., 2002). Other mechanisms raising from the modified two-stream instability (triggered by the relative drift between incoming electrons and incoming ions within the foot region of the front) for oblique shocks (Scholer et al., 2003) may also be responsible for the nonstationarity of the shock front as discussed in Sect. 5.

## 4.3 Magnetic foot

The left panel of Fig. 10 displays the distribution of the magnetic foot
thickness for the 96 shock crossings by any individual spacecraft versus the
foot thickness (normalized with the upstream ion gyroradius *ρ*_{ci}),
whereas the right panel shows the maximal thickness among the four
satellites for each selected shock crossed by the quartet (labeled with the
numbers on the horizontal axis) versus the foot thickness normalized with
*ρ*_{ci}.

First, the distribution (Fig. 10a) clearly shows that the foot thickness
is always found less than the upstream gyroradius. Second, most of the foot
thicknesses (81 %) are found to be less than 0.4*ρ*_{ci,us}, and
the median value is 0.2*ρ*_{ci,us}. Most of the observed shocks
are characterized by a foot with a thickness (${L}_{\mathrm{foot}}<\mathrm{0.1}{\mathit{\rho}}_{\mathrm{ci},\mathrm{us}}$), indicating that the foot width rarely reaches its maximal
value. The literature provides different theoretical determinations of the
foot thickness. Gosling and Robson (1985) used the results of Schwartz et
al. (1983) to show that for an arbitrary angle ${\mathit{\theta}}_{{B}_{n}}$, the upstream
extent of the foot is

where

and *θ*_{vn} is the angle between the shock normal and the upstream
solar wind velocity vector.

Another determination was given by Livesey et al. (1984) as

For a strictly perpendicular shock $({\mathit{\theta}}_{{B}_{n}}=\mathrm{90}{}^{\circ})$ and a normal
incident upstream solar wind (${\mathit{\theta}}_{\mathrm{vn}}=\mathrm{0}{}^{\circ})$, the foot width
reaches the distance for a reflected ion at the time of its turn-around
defined by $\mathrm{d}{x}_{n}/\mathrm{d}t=\mathrm{0}$, where *x*_{n} is the coordinate of the ion
along the normal, given by Woods (1969, 1971):

The values of *d* obtained from Eqs. (1)–(2) are shown by red points in
Fig. 10b for each shock event. For each event, the blue value with error
bar is the largest experimental foot thickness for one among the four
satellites. The horizontal dashed light blue line shows the theoretical
value given by Eq. (4) and clearly stresses that the maximal experimental
foot thickness is usually below the 90^{∘} critical value and the
value obtained from the experimental derivation of ${\mathit{\theta}}_{{B}_{n}}$ and
*θ*_{vn} (considering the error bars). Thus, for each specific shock
crossing and associated parameters, the above two theoretical values which
are supposed to be fixed by the two aforementioned angles (and thus not
varying with time) can be generally considered an upper bound of
the observed “instantaneous” foot thickness.

## 4.4 Comparison with numerical simulation results

To compare more precisely with numerical simulation results, two-dimensional
PIC simulations (where both ions and electrons are treated as individual
macroparticles) have been performed like those of previous studies
(Lembège and Savoini, 1992; Lembège et al., 2009), where the planar
shock is initialized by a magnetic piston (applied current pulse).
Therefore, the shock geometry is always defined in the upstream frame: the
shock propagates along the *x* direction. Periodic conditions are used along
the direction of the planar shock front (*y* axis). Herein, the shock is
strictly perpendicular (${\mathit{\theta}}_{{B}_{n}}=\mathrm{90}$^{∘}) where the
upstream magnetostatic field *B*_{0} is along the *z* axis and propagates within
the (*x*−*y*) simulation plane; this perpendicular shock is used as a reference
case. All quantities are dimensionless, are indicated by a tilde “∼”, and are normalized as follows: the spatial coordinate is
$\stackrel{\mathrm{\u0303}}{x}=x/\mathrm{\Delta}$; velocity $\stackrel{\mathrm{\u0303}}{v}=v/\left({\mathit{\omega}}_{\mathrm{pe}}\mathrm{\Delta}\right)$; time $\stackrel{\mathrm{\u0303}}{t}={\mathit{\omega}}_{\mathrm{pe}}t$, electric field $\stackrel{\mathrm{\u0303}}{E}=eE/\left({m}_{e}{\mathit{\omega}}_{p}^{\mathrm{2}}\mathrm{\Delta}\right)$; and magnetic field
$\stackrel{\mathrm{\u0303}}{B}=eB/\left({m}_{e}{\mathit{\omega}}_{p}^{\mathrm{2}}\mathrm{\Delta}\right)$. The parameters *e*, *m*_{e}, Δ, and *ω*_{pe} are,
respectively, the electric charge, the electron mass, the numerical grid size,
and the electron plasma frequency. These definitions are identical to those
used in previous 1D PIC (Lembège and Dawson, 1987) and 2D PIC
simulations (Lembège and Savoini, 1992). The plasma conditions and shock
regime used herein are similar to those used in Lembège et al. (2009).
All basic parameters are summarized as follows: the plasma
simulation box has 6144×256 grids with a spatial resolution $\mathrm{\Delta}=\mathrm{\Delta}x=\mathrm{\Delta}y=\mathrm{\Delta}z=\mathrm{1}/\mathrm{60}$ ($\stackrel{\mathrm{\u0303}}{c}/{\stackrel{\mathrm{\u0303}}{\mathit{\omega}}}_{\mathrm{pi}}$) = $\mathrm{1}/\mathrm{3}(\stackrel{\mathrm{\u0303}}{c}/{\stackrel{\mathrm{\u0303}}{\mathit{\omega}}}_{\mathrm{pe}})$ (where $\stackrel{\mathrm{\u0303}}{c}/{\stackrel{\mathrm{\u0303}}{\mathit{\omega}}}_{\mathrm{pi}}$ and $\stackrel{\mathrm{\u0303}}{c}/{\stackrel{\mathrm{\u0303}}{\mathit{\omega}}}_{\mathrm{pe}}$ are the upstream ion and
electron inertial lengths, respectively), which is high enough to involve all
microstructures of the shock front. Initially, the number of particles per
cell is 4 for each species. Velocity of light $\stackrel{\mathrm{\u0303}}{c}=\mathrm{3}$, and mass ratio
of proton and electron ${M}_{\mathrm{i}}/{m}_{\mathrm{e}}=\mathrm{400}$. To achieve reasonable run
times and simulation domains, a ratio of ${\stackrel{\mathrm{\u0303}}{\mathit{\omega}}}_{\mathrm{pe}}/{\stackrel{\mathrm{\u0303}}{\mathit{\omega}}}_{\mathrm{ce}}=\mathrm{2}$ has been used
as in Hada et al. (2003) and Scholer and Matsukiyo (2004). The
electron-to-ion temperature ratio is ${T}_{\mathrm{e}}/{T}_{\mathrm{i}}=\mathrm{1.58}$; upstream ions and
electrons are isotropic so that ${\stackrel{\mathrm{\u0303}}{v}}_{\mathrm{thi}}={\stackrel{\mathrm{\u0303}}{v}}_{\mathrm{thi},x,y,z}$ and
${\stackrel{\mathrm{\u0303}}{v}}_{\mathrm{the}}={\stackrel{\mathrm{\u0303}}{v}}_{\mathrm{the},x,y,z}$, respectively. The ambient magnetic
field is ${\stackrel{\mathrm{\u0303}}{B}}_{\mathrm{0}}=\mathrm{1.5}$. The shock has an averaged alfvénic Mach
number ${M}_{\mathrm{A}}={\stackrel{\mathrm{\u0303}}{v}}_{\mathrm{shock}}/{\stackrel{\mathrm{\u0303}}{v}}_{\mathrm{A}}=\mathrm{5.06}$, where the upstream Alfvén velocity ${\stackrel{\mathrm{\u0303}}{v}}_{\mathrm{A}}$ is
equal to 0.075, and the shock velocity ${\stackrel{\mathrm{\u0303}}{v}}_{\mathrm{shock}}=\mathrm{0.38}$. The ratio
$\stackrel{\mathrm{\u0303}}{\mathit{\beta}}$ of upstream plasma thermal pressure to magnetic field
pressure is taken as ${\stackrel{\mathrm{\u0303}}{\mathit{\beta}}}_{\mathrm{i}}=\mathrm{0.10}$ for protons and ${\stackrel{\mathrm{\u0303}}{\mathit{\beta}}}_{\mathrm{e}}=\mathrm{0.16}$ for electrons. For these initial conditions, all other upstream
plasma parameters are detailed in Table 1 for both electrons and protons.

In present plasma conditions, cycles of the shock front self-reformation are
shown as in previous studies (Lembège and Dawson, 1987; Lembège
and Savoini, 1992; Lembège et al., 2009). An enlarged view of the time
stack plot of the (*y*-averaged) main magnetic field component is shown over
one cycle in Fig. 11a. Note that the local direction of the front normal
versus the upstream magnetostatic field is varying along a front ripple.
Then, considering an average along the shock front (*y* axis) is equivalent to
averaging over these local normal directions and agrees with the method used
in experimental data for determining the normal direction of the shock front
crossed by the Cluster tetrahedral configuration for small satellite
inter-distance (i.e., average over local normal directions given individually
by each satellite).

As shown in previous studies, the self-reformation is mainly characterized by
(i) a strong cyclic magnetic field amplitude variation at the overshoot with
a time period ${\stackrel{\mathrm{\u0303}}{\mathit{\tau}}}_{\mathrm{ref}}$ (=1523) on the order of $\mathrm{1}/\mathrm{3}{\stackrel{\mathrm{\u0303}}{\mathit{\tau}}}_{\mathrm{ci}}$ (where ${\stackrel{\mathrm{\u0303}}{\mathit{\tau}}}_{\mathrm{ci}}=\mathrm{5027}$ is the upstream ion
cyclotron period) so that several self-reformations can take place within
one upstream ion cyclotron period; (ii) a temporal anticorrelation of the ** B** amplitude measured at the foot and at the overshoot, respectively, and
(iii) a strong time variability of the shock front width. These features
persist quite well even when using a realistic mass ratio as shown by
Lembège and al. (2013a, b); in particular, the self-reformation
cyclic period does not depend almost on the mass ratio. Moreover, the
features of the other self-reformation process due to the MTSI (for slightly
oblique shocks, see Sect. 1) also persist for realistic mass ratio as shown
by Scholer and al. (2003).

### 4.4.1 Results on the ramp thickness

Herein, the spatial ramp width is identified within the shock front by a
linear fit defined in the steepest part of the magnetic field gradient
(Fig. 11b). However, the procedure to define this width slightly differs
from that used for Cluster experimental data in Sect. 2. Presently, its
lower bound (dashed line B) is defined where the ** B** amplitude departs clearly
(due to the foot region) from this linear fit. On the other hand, its
upper bound (dashed line C) is defined where the B profile departs clearly
(due to the proximity of the overshoot) from this linear fit. We do not use
the overshoot as the upper bound since it is polluted by reflected ions
as these gyrate and penetrate downstream after being once reflected at the
ramp (Leroy et al., 1982); then this would overestimate the ramp width. On
the other hand, let us note that using the mean downstream

**amplitude as a reference (as done for experimental data analysis in Sect. 3) may be a source of inaccuracy when applied to the present numerical simulation results. Indeed, the size of the downstream region is not long enough to deduce a precise estimate of the averaged downstream**

*B***amplitude. In the**

*B***amplitude of Fig. 11b, these lower and upper bounds are, respectively, located at $\stackrel{\mathrm{\u0303}}{x}=\mathrm{3755}$ and 3745 which provides a ramp thickness ${\stackrel{\mathrm{\u0303}}{L}}_{\mathrm{ramp}}=\mathrm{10}$. Repeating the same measurement procedure at different times within the self-reformation cycle allows us to prove that the ramp thickness stays always very narrow around a (time-averaged) value of ${\stackrel{\mathrm{\u0303}}{L}}_{\mathrm{ramp}}=\mathrm{3}\stackrel{\mathrm{\u0303}}{c}/{\stackrel{\mathrm{\u0303}}{\mathit{\omega}}}_{\mathrm{pe}}$ (Fig. 11c); the width of the ramp is almost independent of time and of the strong fluctuations of the maximum**

*B***amplitude at the overshoot (not shown herein), which is mainly driven by reflected ions (Leroy et al., 1982). Since one has to compare statistical results of experimental observations with simulations, it is important to clarify the following points: (i) considering a perpendicular shock represents a reference case in the sense that the ramp is expected to be the thinnest for 90**

*B*^{∘}, as compared with oblique cases (lower than 90

^{∘}), since indeed whistler wave emission (precursor) in oblique shocks tends to extend the thickness; (ii) herein, the concerned simulation is based on a relatively low ${\stackrel{\mathrm{\u0303}}{\mathit{\beta}}}_{\mathrm{i}}$ value (= 0.10) or equivalently a high ratio ${\stackrel{\mathrm{\u0303}}{v}}_{\mathrm{shock}}/{\stackrel{\mathrm{\u0303}}{v}}_{\mathrm{thi}}$ (= 31.66), which fits with the range of experimental conditions where data sets of shock crossing have been chosen (Fig. 8c–d); (iii) over a full self-reformation cyclic time period, the shock front covers a distance of $\mathrm{\Delta}\stackrel{\mathrm{\u0303}}{x}=\mathrm{597}$ (or equivalently $\mathrm{9.8}\stackrel{\mathrm{\u0303}}{c}/{\stackrel{\mathrm{\u0303}}{\mathit{\omega}}}_{\mathrm{pi}}$). In the case study shown in Fig. 6c, the satellites inter-distances along the normal are, respectively, $\mathrm{1.4}c/{\mathit{\omega}}_{\mathrm{pi}}$ for C4–C2, $\mathrm{1.6}c/{\mathit{\omega}}_{\mathrm{pi}}$ for C2–C1, and $\mathrm{2.6}c/{\mathit{\omega}}_{\mathrm{pi}}$ for C1–C3, which makes the total distance for the shock crossing of $\mathrm{5.6}c/{\mathit{\omega}}_{\mathrm{pi}}$; (iv) shock curvature effects and front rippling of the shock front have been neglected herein, in order to approach the experimental conditions where the inter-distance between satellites is small. The

*y*averaging of the simulated planar shock is in agreement with the hypothesis of considering locally a planar shock front in experimental data for estimating the relative speed of each satellite versus the shock velocity. Then one can extract at present the width of the fine structures (foot and ramp) of the shock front mainly along the shock normal with a good accuracy. Moreover, in contrast with the methodology used for experimental data (Sect. 2), it is not necessary to use herein two different levels of identification (“visual” and “automatic”) for defining the upper and lower bounds of each microstructure (ramp and foot), since profiles have been already smoothed out enough by the

*y*averaging.

The variation of the ramp width versus time reported in Fig. 11c shows that three successive time ranges can be defined where, respectively, the width decreases (range i defined by $\stackrel{\mathrm{\u0303}}{t}<\mathrm{3456}$), very slightly decreases (range ii defined by $\mathrm{3456}<\stackrel{\mathrm{\u0303}}{t}<\mathrm{4400}$), and increases (range iii defined by $\stackrel{\mathrm{\u0303}}{t}>\mathrm{4400}$) as represented by pink, blue, and yellow areas, respectively. Then, the width stays almost constant during a large time range (ii). Within this range, the width reaches a lower-bound value around $\mathrm{3}c/{\mathit{\omega}}_{\mathrm{pe}}$ (dashed–dotted red line), which can be used as a reference scale in the comparison with experimental data instead of comparing exact scales measured at a given crossing time of the shock. In order to analyze the whole-time variation of the ramp width in detail, it can be associated with that of the foot and with ion phase space as described in Sect. 4.4.2.

### 4.4.2 Results on the foot thickness

Figure 11d shows the time variation of the foot width issued
from the same PIC simulation. The upstream edge of the foot (vertical dashed
line A in Fig. 11b) is defined as the location where the magnetic field
has increased by 6.67 % over its upstream value (Burgess et al., 1999;
Yang et al., 2009, 2011). The value of 6.67 % has been determined as
corresponding to the maximum amplitude in the magnetic field fluctuations
measured upstream (which is sensitive to the particle number per cell).
Then, the amplitude of the upstream magnetic field turbulence is below the
value (1 + 6.67 %) ×*B*_{0} in our simulations.

The time variation of the foot width can be detailed with the help of the three time intervals defined for the ramp thickness in Sect. 4.4.1 and is associated with the ramp as follows. In range (i), the foot width increases in anticorrelation with the ramp variation; at that time, reflected ions are accelerated at the ramp and only initialize their gyromotion (not shown herein). The range (ii) (where the ramp width slightly decreases) includes three successive phases for the foot dynamics: one (ii-a) where the foot width is constant ($\mathrm{3456}<\stackrel{\mathrm{\u0303}}{t}<\mathrm{3984}$), another (ii-b) where the foot width strongly increases ($\mathrm{3984}<\stackrel{\mathrm{\u0303}}{t}<\mathrm{4176}$), and a last one (ii-c) where the foot width is still increasing. But, in addition, a secondary foot can be identified upstream (blue curve for $\stackrel{\mathrm{\u0303}}{t}>\mathrm{4176}$); a double foot appears as detailed below. Finally, in range (iii) ($\stackrel{\mathrm{\u0303}}{t}>\mathrm{4416}$), the foot width reaches a maximum value (${L}_{\mathrm{foot}}/{\mathit{\rho}}_{\mathrm{ci},\mathrm{us}}$) = 0.6, which remains constant at later times while the ramp thickness starts increasing.

A detailed analysis of the ion phase space (not shown here) at these corresponding time intervals allows us to interpret more precisely the time variation of both ramp and foot thicknesses. In range (i) (i.e., $\stackrel{\mathrm{\u0303}}{t}<\mathrm{3456}$), the ramp (named ramp-1) is freshly formed from the steepening of the foot resulting from the previous self-reformation and the foot in panel (d) is only due to the old reflected ions (previous self-reformation) still located upstream of the new ramp-1 while accomplishing their full gyration (before being transmitted downstream); this steepening corresponds to the decrease of the ramp width (range i in panel c). In range (ii-a), ramp-1 starts to accelerate and reflect new upstream ions, which add to old reflected ions which did not reach the downstream region yet. Then, the local foot (named foot-1) is composed of two (old and new) reflected ion populations (reflected at two successive reformation cycles). During this acceleration phase, the energy of macroscopic fields at the ramp is transferred to newly reflected ions, which smooths the local steepening, and the ramp-1 width slightly decreases only. Within the range (ii-b), all old reflected ions have reached the downstream region; only freshly reflected ions are present upstream of the ramp, continue their gyromotion, and contribute to foot-1. Consequently, the foot-1 width strongly increases as mainly carried by these newly reflected ions. Correspondingly, the width of ramp-1 still slightly decreases. But, more and more new ions are reflected and accumulate in time, and a local new foot (named foot-2 ) builds up. This ion accumulation is large enough so that the upstream edge of this new foot-2 steepens and becomes a new ramp (named ramp-2, not shown in panel d) which starts reflecting new ions; let us mention that the width of ramp-2 cannot be precisely identified before $\stackrel{\mathrm{\u0303}}{t}<\mathrm{4368}$ by using the best linear fit (as in Fig. 11b) since this part of the front microstructure is still mainly dominated by the growing foot (steepening is not strong enough in the upstream edge of foot-2 within this time range). This new foot-2 (blue curve in panel d) co-exists with the old foot-1 (red curve) within the same time interval $\stackrel{\mathrm{\u0303}}{t}>\mathrm{4176}$. Simultaneously, the amplitude of the new overshoot (not shown here) associated with the new ramp-2 increases, and the field gradient between the old and the new overshoot becomes weaker. Therefore, the ramp-1 width increases at a later time (time range iii). For $\stackrel{\mathrm{\u0303}}{t}>\mathrm{4608}$, the old ramp-1 is totally absorbed into the shock profile (between the old and the new overshoots), and its width cannot be identified precisely.

Then, the shock front may acquire a multi-peak profile including traces of old and new successive ramps (not to be confused with emission of large amplitude whistler waves emitted from the main ramp). The width of the whole shock front is the summation of the ramp and the feet contribution and can be estimated from the upper edge of the new foot-2 to the lower edge of the old ramp in the front. Present results provide maximum value measured at the final stage of self-reformation cycle (${\stackrel{\mathrm{\u0303}}{L}}_{\mathrm{shock},\mathrm{max}}=\mathrm{176.3}=\mathrm{2.93}\stackrel{\mathrm{\u0303}}{c}/{\stackrel{\mathrm{\u0303}}{\mathit{\omega}}}_{\mathrm{pi}}$ at $\stackrel{\mathrm{\u0303}}{t}=\mathrm{4608}$). Let us stress that this value represents an upper bound of the shock front width and not a common measurement of the front width itself.

This section is dedicated to comparing the present results with those issued from previous studies. The main emphasis is given not only on the agreement or disagreement observed between the different results but also – and even more importantly – on the strategy used in previous studies for “extracting” the spatial width of the shock front microstructures. We will distinguish previous studies dedicated to measurements of the ramp and of the foot thicknesses.

## 5.1 Spatial measurements of the ramp thickness

### 5.1.1 Newbury and Russell (1996)

Most studies based on the analysis of experimental data issued from ISEE-1
and ISEE-2 satellites indicate a scaling of the ramp width within the ion
inertial length. In a very detailed analysis of a single shock crossing,
Scudder et al. (1986) have reported the ramp thickness to be $\mathrm{0.2}c/{\mathit{\omega}}_{\mathrm{pi}}$, a measurement which was based on an exponential fit of the
foot–ramp transition. By using the same fit technique, Russell and Greenstadt (1979) have measured a slightly thicker ramp of about $\mathrm{0.4}c/{\mathit{\omega}}_{\mathrm{pi}}$
in an initial study of ISEE bow shock observations. Later on, Newbury and
Russell (1996) analyzed seven nearly perpendicular shocks (${\mathit{\theta}}_{{B}_{n}}>\mathrm{80}$^{∘}) and found a range of ramp
widths (based on a linear fit to the ramp transition) from 0.5–0.8 $c/{\mathit{\omega}}_{\mathrm{pi}}$. However, in one case the ramp width was particularly thin $\mathrm{0.05}c/{\mathit{\omega}}_{\mathrm{pi}}$ (= $\mathrm{2}c/{\mathit{\omega}}_{\mathrm{pe}}$). To the knowledge of the
authors, it was the first time that such a thin ramp had been observed
associated with the terrestrial shock. All the observations lead to the
following statements:

- a.
In contrast with the tentative explanations proposed at that time (summarized in Newbury et al., 1998), this very thin ramp ($\mathrm{2}c/{\mathit{\omega}}_{\mathrm{pe}}$) takes a full meaning herein and is in quite good agreement with the present statistical results. It represents quite well a potential signature of the self-reformation process which allows the ramp to have a very small thickness (a few $c/{\mathit{\omega}}_{\mathrm{pe}}$).

- b.
One question arises. Why do most previous studies show mainly a ramp width scaling with a noticeable part of the ion inertial length (except the very narrow ramp mentioned above), which is in contrast to the present results? Several answers can be proposed. First, the method commonly used in previous studies and based on exponential fitting to the foot–ramp region is not appropriate to measure carefully the ramp and foot thickness, respectively, since both fine structures were mixed together. This fitting methodology is a source of important errors. Second, the solar wind conditions corresponding to the set of shock crossings chosen at that time need to be verified carefully. Indeed, as

*β*_{i}is relatively low (*β*_{i}=0.17 as in Hada et al. (2003), or equivalently ${v}_{\mathrm{sh}}/{v}_{\mathrm{thi}}$ equals several decades as in Scholer et al., 2003), the reflected ions describe a focused (narrow) beam during their gyration. These maintain a well coherent gyromotion which forces them to accumulate at a certain distance from the ramp and to initialize the foot. The growth of the foot separates clearly from the ramp and is characterized by a trapping loop in the ion phase space; self reformation takes place, and the front is nonstationary.

In contrast, as *β*_{i} is relatively high (*β*_{i}=0.35
as in Hada et al., 2003, or ${v}_{\mathrm{sh}}/{v}_{\mathrm{thi}}$ equals a few units as in
Scholer et al., 2003), the reflected ions rapidly diffuse as they start
their gyromotion; these lose their large coherent motion and spread out
within the whole front (no clear ion trapping loop). The foot grows up but
does not separate from the ramp. Then, ramp and foot are mixed, and a larger
thickness of the ramp–foot region is expected as shown in PIC simulations
of Lembège et al. (2013a, b). Then, no self-reformation can take
place, and the shock front is stationary.

### 5.1.2 Newbury et al. (1998)

At the ISEE-1 and ISEE-2 time, the ramp was usually characterized by two different scales: (i) a large scale (or global ramp width) within which the main transition from upstream to downstream magnetic fields takes place and (ii) a thinner subramp scale which contains steep jumps in the magnetic field with amplitudes sometimes comparable to the overall change in the magnetic field at the shock. One conclusion (Newbury et al., 1998) was that both scales are characteristic of the quasi-stationary shock profile (which – at that time – was considered stationary within the ion gyroperiod). More precisely, Newbury et al. (1998) have analyzed a set of 20 shock crossings and found that the width of the overall ramp transition is typically within the range 0.5–1.5 $c/{\mathit{\omega}}_{\mathrm{pi}}$, which is quite large as compared with our present measurements. This difference can be easily explained by the fact that the authors have defined the ramp thickness based on a linear fit of the total magnetic field profile from the foot to the overshoot, which enlarges the estimate of the ramp thickness, as compared with the present method used in Sects. 3 and 4.

Cluster data and present statistical results allow us to correct this view within the frame of the intrinsic shock front self-reformation. The so-called “large scale” of the ramp presents a large width variability (extending from a part of the ion inertia length to a few electron inertia lengths as displayed in Fig. 9a), which was not observed at that time for the reason mentioned above. But, simultaneously, the so-called “small scales” can result from instability developing with the foot region as the ECDI, which represents Electron Cyclotron Drift Instability (Muschietti and Lembège, 2006, 2013) or MTSI (Scholer et al., 2003; Matsukyio and Scholer, 2003; Muschietti and Lembège, 2017), for instance, and can propagate (convection effects). In the present work, the use of a linear fit applied within the ramp region only (as described in Sect. 3) allows us to average these local small-scale fluctuations and to measure the ramp width with minimizing errors. Analyzing small-scale field fluctuations (as those also observed within the ramp in Figs. 3 and 5) requires a further investigation which will be presented elsewhere.

### 5.1.3 Bale et al. (2003)

From the spacecraft floating potential measured on board the four Cluster
satellites, Bale et al. (2003) have determined the electron plasma density
and studied the macroscopic density transition scale at 98 crossings of the
quasi-perpendicular terrestrial bow shock. This first tentative clue for measuring
the shock transition width from Cluster data was attractive but contains
several limitations for the following reason: a hyperbolic tangent function
has been fitted to each density transition in order to capture the main
shock transition but no microstructures of the front – as foot, ramp,
or overshoot – have been identified and scaled. Such a fit partially includes
parts of the shock front outside the ramp itself so that it cannot apply to
determine the ramp thickness with acceptable accuracy since both ramp and
foot structures are not separated. This technique takes into account only
the widest transition scale at the shock front, which overestimates the ramp
width and restricts drastically its application. Then, the conclusions
stating that, for high Mach number shocks (including the range
*M*_{A} = 4–5 as that considered in the present work), only the convected
gyroradius is the preferred scale for the shock density transition are
strongly questionable since the real ramp is much thinner. This resulting
scale corresponds to the scale of the foot rather than that of the ramp, and
no conclusive statements can be obtained.

On the other hand, in the light of Cluster data, looking for an estimate of the shock transition presents, nowadays, a limited interest, since recent results show that terrestrial shock is rather nonstationary and a “unique” typical spatial scaling must be replaced by some interval or bounds of variation (lower bound and upper bound) within which the spatial scales of the fine structures can vary.

Figure 12 helps us to better compare our results with those by Bale et al. (2003), which have been reproduced in Fig. 12a, b, and d. The same
representation as in Fig. 12b and d has been used for Fig. 12c and e
to plot the front thickness computed as the sum of the ramp and the foot
thicknesses from our methodology versus the magnetosonic Mach number
*M*_{ms}. The pink area in Fig. 12b illustrates the range of *M*_{ms}
explored from the present study. Figure 12c reveals that in this range of
*M*_{ms} values no clear dependence considering the large error bars (as on
above Fig. 12b) can be identified from the present study. It would be
obviously impossible here to conclude that the front thickness simply
increases with *M*_{ms} and conversely the best fit would conclude here that
there is a trend to decrease. Our results are therefore in strong
contradiction with conclusions of Bale et al. (2003). Moreover, if we
consider another *M*_{ms} range of similar extension as the one shown in
Fig. 12c from our study and highlighted by the green area in Fig. 12b, a
similar representation (not shown here) would conclude to exactly the
opposite to what the dotted line in Fig. 12b shows, considering again the
large error bars. This illustrates again the impossibility to make a simple
scaling of the front thickness by a single parameter as the magnetosonic
Mach number. Figure 12e shows that the front thickness normalized by the
downstream gyroradius is more or less consistent with the results of Bale et
al. (2003) shown in Fig. 12d. There is a trend there to decrease with
*M*_{ms} increase. As mentioned in the present study, the use of the
so-called “density transition scale” by Bale et al. (2003) shown in Fig. 12a is inappropriate since it mixes the time variability of the ramp and the
ion foot. They also mention a stationary shock from their Fig. 1. But,
this figure does not show the highest temporal resolution of the magnetic
field data but only corresponds to five values per second. For many shock
crossings used in the present study, the profiles displayed at 5 Hz look
very similar, whereas the highest-time-resolution profiles clearly reveal
different features (as illustrated in our Fig. 6).

### 5.1.4 Krasnoselskikh et al. (2002)

Krasnoselskikh et al. (2002) have proposed another mechanism as a possible
source of nonstationarity of the shock front (so-called gradient
catastrophe), where the shock appears as a balance between nonlinear and
dispersive effects only. In this mechanism, the transition to
nonstationarity is characterized by the lack of the phase standing whistler
wave train inside the shock front. This process takes place for oblique
quasi-perpendicular shock (for a direction ${\mathit{\theta}}_{{B}_{n}}$ not too far from
90^{∘}) as the Alfvén Mach *M*_{A} is above a certain critical Mach
number given by ${M}_{\mathrm{nw}}=(\mathrm{1}/\mathrm{2}{)}^{\mathrm{1}/\mathrm{2}}({M}_{\mathrm{i}}/{m}_{\mathrm{e}}{)}^{\mathrm{1}/\mathrm{2}}\mathrm{cos}{\mathit{\theta}}_{{B}_{n}}$; this
condition can be equivalently expressed for a fixed *M*_{A} as the direction
${\mathit{\theta}}_{{B}_{n}}$ is below a critical angular value. In this case, the
nonlinear steepening of the wave train cannot be balanced by the dispersion
effects alone. However, as mentioned in Sect. 1, this theoretical mechanism
has severe limitations since (i) it is based on a 1D model only and (ii) it
excludes any dissipative effect. Indeed, reflected ions (which play a key
role in supercritical Mach regime) are neglected, and their impact on the
shock dynamics – and in particular on the temporal fluctuations of the
shock front microstructures which is our center of interest in the present
paper – is totally absent. Because of the above severe limitations, this
process is still a source of controversy and is not considered herein.

### 5.1.5 Lobzin et al. (2007)

Nevertheless, a further study made by Lobzin et al. (2007) has proposed the
gradient catastrophe process as being at the origin of the shock front
nonstationarity observed by Cluster on 24 January 2001. While the front
nonstationarity is quite clear in the experimental data which show quite
different shock front profiles of the magnetic field crossed by the four
satellites of Cluster, the proposed interpretation stays quite questionable
for the following reasons: (i) the overall analysis is based on one shock
crossing only (no statistical analysis has been performed), (ii) no
procedure detailing the transfer from time to spatial scaling of the shock
front (in particular focused separately on the ramp or foot structures) has
been indicated, so one ignores the percentages of errors underlying the
spatial field profiles measurements which are not shown; (iii) no mapping
and/or basic information have been provided on the 3D disposal and
inter-distance of the satellites, so one ignores whether the four
satellites cross the same shock front within the same or different
successive self-reformation cycles; (iv) only one measurement of the ion
density showing some fluctuations has been presented which is not enough for
confirming that it could be due to the gradient catastrophe process.
Moreover, note that such similar density fluctuations have been also
measured quantitatively versus time in previous numerical simulations
(Lembège and Savoini, 1992; Yang et al., 2009) but have been attributed
as being due to the self-reformation process fed by the accumulation of
reflected ions and not to the gradient catastrophe process. Similar
self-reformations have been also obtained as supported by the MTSI for an
obliquely propagating shock (Comisel et al., 2011); (v) a deeper analysis
shows that the upstream ion temperature used in this paper is not the
correct one since the CIS instrument was in magnetospheric mode (see Sect. 2), so the moment calculations provide a large overestimate of the solar
wind proton core temperature. Indeed, the determination of the upstream ion
thermal velocity requires a delicate procedure and is of central interest
since the stationarity or nonstationarity of the shock front is strongly
dependent on the ratio ${v}_{\mathrm{sh}}/{v}_{\mathrm{thi}}$ (Scholer et al., 2003)
or similarly on the ratio *β*_{i} (defined as the ion kinetic energy
over magnetic energy) (Hada et al., 2003). When using the solar proton
temperature from the ACE satellite (4.5 eV thermal energy), the ion beta
found is 0.6 instead of the value of 2.0 reported by Lobzin et al. (2007).

### 5.1.6 Comisel et al. (2011)

The same data of Cluster measured on 24 January 2001 has been re-examined in
detail by Comisel et al. (2011) and re-interpreted quite differently by
using PIC simulations in plasma conditions and Mach number regimes chosen to
be appropriate with experimental conditions. Basically, the authors have
shown that the self-reformation is quite well recovered but is not
controlled by the gradient catastrophe process (dispersive effects only)
mentioned above but rather by the self-reformation mechanism fed up by the
MTSI which is an indirect consequence of the ion reflection (dissipative
effects which have been neglected in Krasnoselskikh et al., 2002). Indeed,
for slightly oblique shocks (out of 90^{∘}), the MTSI develops
between the incoming electrons and incoming ions, with a growth rate large
enough to develop during the gyration of the reflected ions (Scholer and
Matsukiyo, 2004). These authors have shown that for a nonrealistic mass
ratio, the self-reformation is still controlled by the collection of
reflected ions at the upstream edge of the foot as in Lembège and
Savoini (1992), since the MTSI has a weak growth rate and has no impact on
the nonstationary dynamics of the shock front. In contrast, for realistic
mass ratio, the growth rate is much larger, and MTSI can be easily excited,
which leads to ion phase mixing and thermalization. Then, the ion pressure
increases considerably locally somewhere within the foot itself (and not at
the edge of the foot) with associated building up and overtaking of the
magnetic field. A new shock ramp builds up within the foot which initiates
to reflect new incoming ions and a cyclic reformation is initialized. The
cyclic period is lower than the one associated with the self-reformation due
to the accumulation of reflected ions (as in Lembège et Savoini, 1992), since the process takes place before ions accomplish their full
gyration. More precisely, by using the appropriate conditions of the 24 January 2001 shock crossing in the PIC simulations, Comisel et al. (2011)
have shown that the waves triggered by this instability are of whistler type and
have phase velocities directed downstream in the shock frame, and the
associated Poynting flux (and wave group velocity) is also directed in the
downstream direction. However, as these approach the density and magnetic
field overshoot, the waves are refracted; as a consequence, the Poynting
flux changes direction and is directed upstream in the shock frame. In
summary, there is no indication of a phase standing linear or nonlinear
whistler precursor produced by the shock ramp itself in this process. This
scenario does not support the scenario that proposed by Krasnoselskikh et al. (2002),
where a nonlinear whistler precursor is required to initialize the gradient
catastrophe process as a source of the front nonstationarity.

### 5.1.7 Hobara et al. (2010)

A statistical study based on 77 crossings of the terrestrial bow shock (30
by THEMIS (Time History of Events and Macroscale Interactions during Substorms) and 47 by Cluster) has been performed by Hobara et al. (2010) in
order to analyze the ramp scale and the associated gradient width. Their
study claims that the spatial scale of the ramp decreases as the shock
Alfvén Mach number increases. However, detailed comparison with our results
is difficult (almost impossible) at the present time because of important
missing information. (i) No detailed information is provided on the
procedure used for extracting the spatial widths of the ramp from the
temporal experimental data as detailed in present Sect. 2; (ii) the duration
of the ramp crossing has been defined as a time interval between the
upstream edge of the ramp and the maximum of overshoot. However, let us note
that the upstream edge is not defined precisely (see the precaution to account
for in our Sect. 3), and the use of the overshoot can lead to an
overestimate of the ramp width as compared to the method used herein (Sect. 3) since it is partially polluted by reflected ions; (iii) statistical
errors are indicated in their Figs. 2 and 3 only for a range of Mach numbers
and not on individual measurements; (iv) no statistics are shown versus the
direction (${\mathit{\theta}}_{{B}_{n}}$) of the shock front normal; as a consequence, one
ignores how and whether the measurements of the ramp or foot bounds are polluted
by the whistler (either linear or nonlinear), whose emission strongly
depends on the angle ${\mathit{\theta}}_{{B}_{n}}$; (v) no statistics or information is
indicated on the ion *β*_{i} value (which has a strong impact on the
shock front self-reformation) (Hada et al., 2003); (vi) the authors use two
different statistics: one based on the ramp spatial scale (their Fig. 3) and the other based on magnetic ramp spatial gradient scale (their Fig. 4). Moreover, they used a simple theoretical argument (based on dispersive
whistler) to stress that the wavelength *L*_{w} of the linear or nonlinear
whistler varies as ${L}_{\mathrm{w}}\sim \mathrm{1}/{M}_{\mathrm{A}}$. But the fact that
both statistics show that the width of the measured structure decreases as
*M*_{A} increases does not imply that dispersion determines the size of the
magnetic ramp even for supercritical shocks (as discussed later on); (vii) at least, only a very limited number of measurements (whatever the *M*_{A}
value is within the concerned range *M*_{A} = 2–12 in Hobara et al., 2010)
indicate that the ramp width succeeds to reach a few electron inertial
lengths (equal to or lower than $\mathrm{5}\stackrel{\mathrm{\u0303}}{c}/{\stackrel{\mathrm{\u0303}}{\mathit{\omega}}}_{\mathrm{pe}}$, in their Figs. 2 and 3), which is in strong contrast with our
statistical results of Fig. 9a. The lack of statistics versus ${\mathit{\theta}}_{{B}_{n}}$ and *β*_{i} (above points iv and v) and the
absence of precise information on the methodology used in the statistics of
Hobara et al. (2010) (as listed above) could explain this difference.

Moreover, Hobara et al. (2010) deduce that their measurements (in particular
the decrease of the ramp thickness as *M*_{A} increases) show that the
major process responsible for the shock front nonstationarity is the
gradient catastrophe process proposed by Krassnoselskikh et al. (2002)
and Lobzin et al. (2007). However, three main facts contradict this
statement: (i) the first is arguments describing the severe limitations of the
theoretical model (Krassnoselskikh et al., 2002) and the revised analysis
of Comisel et al. (2011) as already described above in the present section, (ii) Hobara et al. (2010) use the overshoot (observed in the set of their
experimental measurements) as an upper bound to define the ramp width, but
the overshoot of supercritical shocks is a clear signature of the reflected
ions as these gyrate downstream after being once reflected at the ramp
(Leroy et al., 1982). Then, a contradiction occurs since dissipation effects
(strongly carried by the reflected ions) have been fully neglected in the
model of gradient catastrophe which cannot support their statements;
(iii) a similar variation of the ramp thickness as *M*_{A} increases has also been
observed in the self-reformation process in PIC simulations (not shown
here), which means that this variation cannot be used as a unique signature
of the gradient catastrophe process. At least, in order to support their
statements, Hobara et al. (2010) recall that PIC simulations evidencing the
self-reformation due to the accumulation of reflected ions at a foot
distance from the ramp (as in Lembège and Savoini, 1992) as well as
due to the MTSI (as in Matsukyio and Scholer,
2006 use low ${\mathit{\omega}}_{\mathrm{pe}}/{\mathit{\omega}}_{\mathrm{ce}}$ ratio, which overestimates the electric field to
magnetic field ratio (in practice, using a realistic ${\mathit{\omega}}_{\mathrm{pe}}/{\mathit{\omega}}_{\mathrm{ce}}$ ratio is very difficult at present time for
computational constraints). If were true, this argument would suggest that
the electric field would be too large and that the self-reformation process
would result from an artifact. However, no quantitative result has been
obtained until now to support such a statement. In contrast, let us remind
the reader that (i) the parametric analysis performed by Lembège et al. (2009)
clearly shows that both hybrid and PIC simulation retrieve the same
self-reformation process of the shock front in similar plasma conditions and
Mach regime, provided that the space grid is small enough (i.e., high
resolution) in hybrid simulations as shown initially by Hellinger et al. (2002); this last result would suggest that the field gradients at the ramp
are important and not the absolute fields amplitude; (ii) electron scales
are neglected in common hybrid simulations (as those used in Hellinger et
al., 2007; Lembège et al., 2009, and references therein), which are
independent of the ratio ${\mathit{\omega}}_{\mathrm{pe}}/{\mathit{\omega}}_{\mathrm{ce}}$. This suggests
that the ratio ${\mathit{\omega}}_{\mathrm{pe}}/{\mathit{\omega}}_{\mathrm{ce}}$ has no direct impact on the
self-reformation. Note that the ramp width may be estimated in terms of
percentages of ion inertial length in hybrid simulations and both in terms
of electron and ion inertial lengths in PIC simulations.

In summary, the measurements of Hobara et al. (2010) do not support the model describing the ramp as an evolving nonlinear whistler wave; neither does the mechanism of the gradient catastrophe process of Krassnoselskikh et al. (2002) as a source of the front nonstationarity.

### 5.1.8 Schwartz et al. (2011)

Schwartz et al. (2011) have determined the scale of the electron temperature
gradient via electron distributions measured in situ by the Cluster
spacecraft and have identified two different scales: when the Mach number is
supercritical (*M*_{A}=3.8) and when the shock propagation is oblique
(${\mathit{\theta}}_{{B}_{n}}=\mathrm{83}$^{∘}). First, the authors found that half of
the electron heating coincides with a narrow layer covering several electron
inertia lengths ($c/{\mathit{\omega}}_{\mathrm{pe}}$) and found an inflated electron
distribution due to primarily the electron filling in or the entrapment in
regions of phase space that would not be accessible. Second, the remaining
solar wind maximum is only present in the smoother increase of the
field which precedes the ramp; this beam is totally destroyed by the time
this electron scale ramp is crossed. The authors found that this scale is
comparable to that deduced from the theoretical limiting case of a wave
capable of phase standing in the incident flow and concluded that this
suggests that supercritical shocks steepen to this whistler limit since
dissipation processes are insufficient to broaden the transition further.

However, several elements of information are missing: (i) the authors mentioned to have used a technique to convert the time series of data to distance along the shock normal similar to that of Schwartz (1998), i.e., the procedure to determine the normal and the velocity of the shock from multi-spacecraft measurements (as in Sect. 2), but did not provide detailed information on the procedure itself, associated errors estimate, or on the definition of the ramp itself (their Fig. 1); (ii) the results are limited to one shock crossing (one spacecraft only), and some attempts for other shock crossings are mentioned, but no statistical results have been shown or summarized; (iii) the observed results cannot lead to the conclusions that dissipation processes are insufficient to broaden the transition further, since once again the key dissipation processes driven by the (reflected) ions are not mentioned or analyzed in the study. Of course, dispersive effects must be considered in the global balance of nonlinear steepening of the front by both dispersive or dissipative effects, but this does not mean that the shock front dynamics are controlled by dispersive effects. Moreover, other sources of field fluctuations may take place in the shock front (such as formation of multi-peaks (signatures of old or new self-reformation (Sect. 4.4.2) and/or whistler waves excited by the MTSI within the front) without invoking any dispersive effect.

### 5.1.9 Yang et al. (2020)

Very recently, Yang et al. (2020) claimed to have identified shock front self-reformation with the help of high-resolution Magnetospheric MultiScale (MMS) satellite data. This study using measured ion phase space together with B profiles clearly shows the importance of dissipation effects carried by the reflected ions. However, the comparison with the results of the present study proves to be quite difficult due to the lack of precise information. While the MMS data show clearly that the crossed shock is nonstationary, a clear proof of the self-reformation is still questionable for the following reasons:

- a.
The whole study is based on one shock crossing only and eventually restricted to a comparison between two satellites since three of them show very similar profiles and appeared to be in a plane nearly parallel to the shock front. No statistical results are shown or even summarized, which could have stressed the ion vortex formation over different steps of its formation.

- b.
The authors mentioned to have used the timing technique (Schwartz, 1998) to determine the normal and the velocity of the shock front from multi-spacecraft measurements. But no information is given on the application of the procedure itself (in each spacecraft frame) or on the estimate of associated errors. The use of typical magnetic field peaks around the overshoot is mentioned but without specifying where in the different time series. The use of the overshoot is quite odd since it is not precise enough (contrary to the middle of the ramp) as a reference point; indeed, it contains superimposed fluctuations and is partially polluted by reflected ions. Moreover, important information equivalent to reference satellite and reference time (as proposed in our Sect. 2.2) are missing. In addition, no information is given on the identification of the ramp itself and on the conversion from the time series to distance profile along the shock normal.

- c.
The analysis mentions a shock ramp of less than 0.3 $c/{\mathit{\omega}}_{\mathrm{pi}}$, which is not precise enough, seems high, and is in contrast with the fact that

*M*_{A}is relatively high (*M*_{A}=10.8). For such a value, one could expect a much narrower ramp width (see statistics in our Fig. 9d). In addition, one ignores (i) how this ramp width has been measured and (ii) the precise values of the ramp width during the shock crossing by each satellite. - d.
The emerging large-scale fluctuations announced as a new ramp for only one satellite may be questionable. The new front is not “mature” enough during the shock crossing, and the precise location of the “new ramp” within these fluctuations is not clearly identified. One can wonder whether it could be the signature of front rippling and/or multi-crossing due to the back and fourth motion of the shock front, which would need a further analysis.

## 5.2 Spatial measurements of the microstructures

Walker et al. (2004) investigated short-scale structures in the electric
field that are observed during crossings of the quasi-perpendicular bow
shock using also data from the Cluster satellites. An example is reproduced
from this paper in Fig. 13a. The structures observed at each Cluster
satellite exhibit large amplitudes, as high as 70 mV/m, and the
authors argue that they make a significant contribution to the overall change in
the potential at the shock front. They have shown that the scale size of
these short-lived electric field structures is on the order of a few
$c/{\mathit{\omega}}_{\mathrm{pe}}$ as shown in their statistics reproduced in Fig. 13c. They
also studied the relationships between the scale size and the upstream Mach
number and ${\mathit{\theta}}_{{B}_{n}}$. They found that the scale size of these
structures decreases with decreasing *β*_{i} and as ${\mathit{\theta}}_{{B}_{n}}$ approaches 90^{∘}.

Interestingly, the comparison of distributions displayed in Fig. 13b (present analysis) and Fig. 13c (Walker et al., 2004) shows that the electric field structures are consistent with microstructures of the ramp since the typical scales found seem smaller. Of course, to be fully conclusive, one would need to compare the size of the electric field structure and of the magnetic ramp for each shock crossing. However, both results seem very consistent. Recently, Dimmock et al. (2019) have shown electron-scale field structures inside the shock ramp from a case study using the observations of only two Cluster spacecraft which were very close to each other, and they proposed that it is associated with the transition to nonstationarity.

## 5.3 Spatial measurements of the foot thickness

As compared with studies focused on the ramp width, previous studies dedicated to the spatial measurements of the foot thickness are in relatively limited number. First observations of the foot have been made by Paul et al. (1965). Woods (1969, 1971) has proposed the reflected ions to account for the foot structure and has estimated a foot width for a strictly perpendicular shock from the turning point distance (Eq. 4 of Sect. 4.3, which is recalled here):

assuming a specular reflection of ions, where *ρ*_{ci,us} is the
upstream ion gyroradius estimated from the bulk velocity of the solar wind
(and not from the ion thermal velocity); the reflection is specular in the
sense that the incident ion's velocity component along the shock normal is
reversed at the shock, while the component perpendicular to the shock normal
remains unchanged. A good agreement has been found with ISEE-1 and ISEE-2 data
by Paschmann et al. (1982) and Sckopke et al. (1983). However, two points
need to be stressed: (i) the measurement has been made from the ramp to
the turning out point of reflected ions for five ISEE-1 and ISEE-2 crossings of
the shock; (ii) the condition of specular reflection is not simple when
applied to oblique shocks, as shown by Livesey et al. (1984), who estimated
the foot thickness for an arbitrary direction, ${\mathit{\theta}}_{{B}_{n}}$, of the shock
normal as in Eq. (3) of Sect. 4.3 that we recall here:

where *θ*_{vn} is the acute angle defined between the incoming solar
wind direction and the normal to the shock front. A good agreement has been
obtained between the experimental measurements (distance from the ramp and
to the turning point of reflected ions for several shock crossings made by
ISEE-1 and ISEE-2) and values deduced from Eq. (1). Moreover, Moses et al. (1985) found that the shock velocity *v*_{sh} in the frame of the spacecraft
can be expressed as

where

The “–” sign refers to a transition from upstream to downstream, the “+”
sign refers to the inverted transition, Ω_{ci} is the upstream ion
gyrofrequency, and Δ*t* is the foot traversal time. Later on, Gosling
and Thomsen (1985) have derived a more general expression for the turnaround
distance *d*_{turning} for arbitrary ${\mathit{\theta}}_{{B}_{n}}$ which differs from Eq. (3)
particularly for ${\mathit{\theta}}_{{B}_{n}}<\mathrm{60}$^{∘} and which
incorporates above Eqs. (1) and (2) of Sect. 4.3. Initial steps of their
derivation of *d*_{turning} are closely similar to the formalism initially
developed by Schwartz et al. (1983) and leads to the following (Gosling and Robson, 1985):

where

and *t*_{1} is the time of the turnaround defined by $\mathrm{d}{x}_{n}/\mathrm{d}t=\mathrm{0}$, where
*x*_{n} is the coordinate of the ion along the shock normal.

Results obtained by Eqs. (3) and (6)–(8) have been compared and analyzed by Gosling and Thomsen (1985).

Since present statistics concern a quasi-perpendicular shock with shock normal
direction range 74^{∘} < ${\mathit{\theta}}_{{B}_{n}}$ < 90^{∘} (Figs. 8 and 9), one can apply and compare Eqs. (6)–(8) to
our statistical results. Above Eqs. (3) to (8) have been obtained within the
frame of a stationary foot where the overall shock front profile (composed
of ramp and foot) is fixed. Values obtained from Eqs. (6)–(8) have been
reported in Fig. 10b (red dots), where each value includes the dependence
of ${\mathit{\theta}}_{{B}_{n}}$ for each shock crossing. Then, results of Fig. 10b
confirm well that Eqs. (6)–(8) provide an upper bound of the foot thickness
for all experimental measurements analyzed herein. Indeed, the conditions
for ion reflection are varying in time. Numerical simulations have already
shown that (i) the density of reflected ions cyclically varies with a
period equal to the self-reformation cycle (formation of ion bursts as
shown in previous studies (Lembège and Savoini, 1992; Yang et al., 2009;
Comisel et al., 2011)); similarly, bursts of electrons (with parallel kinetic
energy) are formed for oblique shocks as long as the self-reformation
persists, i.e., until a certain critical angle (Lembège and Savoini, 2002);
(ii) the shock front variability has also a strong impact on the nature of
the acceleration process, i.e., SSA (shock surfing acceleration) versus SDA (shock
drift acceleration), during their reflection as shown by Yang et al. (2009).

In the same way, a super-upper-bound value of the foot thickness can be obtained from the simplified Eq. (3) defined for a strictly perpendicular shock. The deduced value ${L}_{\mathrm{foot}}/{\mathit{\rho}}_{\mathrm{ci},\mathrm{us}}=\mathrm{0.68}$ (herein the convection bulk velocity of the solar wind is equal to the shock velocity since we are in the rest solar wind reference frame) has been reported in simulation results of Fig. 11d (perpendicular shock). Equation (3) provides a very good upper limit of the time variation of the foot thickness (reported also in Fig. 10b).

In summary, since the shock front is highly nonstationary, no fixed theoretical scale can be provided as a reference in contrast with statements of many previous studies. Present results confirm that considering the whole shock front to determine the transition layer width can be a source of errors and misunderstanding. Instead, (i) a detailed and separate analysis of microstructures (ramp, foot, and later overshoot) is necessary, and (ii) a comparison with a lower-bound value (for the ramp width) and upper-bound value (for the foot width) reveals to have a full and more comprehensive meaning.

## 6.1 About the methodology used for extracting the spatial width of each fine structure

This work presents in detail the different steps necessary to determine carefully and without ambiguity the spatial thicknesses of each fine structure from the magnetic field measurements, which are summarized as follows:

- 1.
An upstream time interval is defined in the time series for each of the four spacecraft, and an average magnetic field is determined. If all average fields agree in direction and magnitude within predefined limits, an unperturbed upstream field

*B*_{0}is obtained for the global shock crossing by the four satellites. - 2.
For each spacecraft, the entry times in the magnetic foot are automatically determined when the values of the components and magnitude exceed the upstream values by a certain value defined from the upstream standard deviations; then one validates by visual inspection that results are not polluted by any upstream disturbance or detached wave packet.

- 3.
A downstream interval is defined to measure the downstream asymptotic value of the magnetic field (

) magnitude.*B* - 4.
For each spacecraft, an automatic procedure is applied on the magnetic field magnitude to determine the entry and exit times from the magnetic ramp. This procedure is initialized by preliminary estimates using the upstream and downstream asymptotic levels and based on a linear regression used only to better define the time interval where the gradient is the strongest with the best correlation coefficient.

- 5.
The exit time from the first overshoot is estimated first by the magnetic field magnitude reaching the downstream asymptotic value for the closest time to the first undershoot and then adjusted by allowing a reasonable variation (for instance 5 %) of the downstream asymptotic value (see Sect. 2, Fig. 3a).

- 6.
The interval variations of the entry and exit times for each microstructure are used to define error bars on them.

- 7.
The values of both the normal to the shock and its velocity in each spacecraft frame are determined using the four-spacecraft timing method. The obtained normal vector

*n*_{0}is then used to determine the general geometry of the shock characterized by the angle ${\mathit{\theta}}_{B{n}_{\mathrm{0}}}$ with the unperturbed upstream field vector*B*_{0}determined above. The error bars on ${\mathit{\theta}}_{B{n}_{\mathrm{0}}}$ come from both the determination of*B*_{0}and*n*_{0}from the timing errors. - 8.
The spatial profile along the normal direction

*n*_{0}is derived from time profiles for each spacecraft in units of upstream ion inertial length, and the microstructure thicknesses are derived in terms of appropriate physical lengths;

The fitting techniques based on exponential or hyperbolic functions and used in previous studies to match a shock front profile is questionable since these lead to mixing spatial scales of the foot and the ramp. Rather, our statistical results state that a linear best fit with appropriate identification of the upper and lower bounds of the temporal time ranges of the ramp and the foot is much more accurate and allows for a precise error estimate on the spatial width of each microstructure.

## 6.2 About comparing experimental with numerical simulation or theoretical results

Simulation of a strictly perpendicular case as presented in Sect. 4 can be considered herein as a reference case allowing us to provide some bound ranges within which statistics of experimental results may be inserted. More precisely, these provide the following information: the time variation of the ramp thickness is relatively limited (almost constant), and one can define a “lower limit” (a few electron inertial lengths) for the ramp width. In contrast, the foot thickness is strongly varying in time, and one can define an “upper limit” provided by Eq. (2) (which simplifies into Eq. 3 for a strictly perpendicular shock).

Moreover, statistical analysis of measurements appears to be much more
essential than the analysis of a single shock crossing only, in order to
gather relevant information on the widths of the front microstructures.
Since no shock crossing will be exactly identical to another, even
after a deep selection of data, we have to collect several shock crossings
in slightly different conditions in terms of Mach number regime, of shock
normal direction, of *β*_{i} plasma conditions, and of orientation of
the shock crossing by the four satellites. In addition, each shock crossing
reveals some variability of fine structures thickness within the front.
Then, no one-to-one correspondence in comparing numerical and experimental
data for each crossing is possible; instead, the use of lower and upper
limits mentioned above reveals to be much more relevant and comprehensive.

## 6.3 About the possible identification of the process responsible for the shock front nonstationarity

Several points need to be emphasized:

- i.
All shock profiles analyzed herein exhibit a foot and overshoot which are clear signatures (in supercritical regime) of the gyration of reflected ions upstream of the ramp and of these same reflected ions that succeed to penetrate downstream after being once reflected at the ramp. Then, dissipation effects carried by these reflected ions need to be fully considered. Among the different mechanisms proposed to account for the shock front nonstationary, only two processes named “self-reformation” include self-consistently (without any approximation) the competition between the nonlinear, dissipative, and dispersive effects and in particular the important role of reflected ions on the shock dynamics (and vice versa). Up to now, one still ignores whether the self-reformation is mainly controlled by the accumulation of reflected ions which is observed for perpendicular and quasi-perpendicular shocks (Lembège et Savoini, 1992) or by the MTSI-1 (Scholer and Matsukyio, 2004; Muschietti and Lembège, 2017), which is triggered only for oblique shocks (out of 90

^{∘}); MTSI-1 refers to the instability excited in the foot region by the relative drift between the incoming electrons and the incoming ions. This open question will require a further analysis which is under investigation. - ii.
Among others, one typical signature of a front self-reformation is the anticorrelation between the time variation of the “new” growing foot and the “old” overshoot as illustrated in Fig. 11a. Indeed, as the amplitude of the new foot increases, new incoming ions start to be reflected, which has an impact in the need for local dissipation at the overshoot located just behind. Then, a clear identification of a given self-reformation process would require an inter-satellite distance such that the four satellites cross the same shock front within its same reformation cycle. This requires a short inter-satellite distance for the quartet. This seems more easily addressed with the Magnetospheric MultiScale (MMS) mission data, though the spacecraft separation is so small that low-scale fluctuations of the shock front (ripples) has a different impact on the shock normal determination. These low-scale ripples have been identified in a single case study by Johlander et al. (2016) and also indicated from the observed variations of the cross-shock potential in another single case study by Hanson et al. (2019).

- iii.
We emphasize the importance of dimensionality effects in simulation studies for identifying what mechanisms can be dominant in the shock front nonstationarity. For a strictly perpendicular propagating shock, both 2D hybrid and 2D PIC simulations have clearly shown the emission of nonlinear whistler waves which stay stationary with the ramp and propagate obliquely with respect to both the shock normal and the upstream magnetostatic field

*B*_{0}(Hellinger et al., 2007; Lembège and al., 2009). This emission holds only as the*B*_{0}field is laying within the simulation plane (and self-reformation is absent) and disappears as*B*_{0}is out of the simulation plane (and self-reformation is present). The source of this whistler emission has not been clearly confirmed yet; ion Weibel instability has been recently proposed as a possible mechanism (Burgess et al., 2016). In other words, the emission of these whistlers seems to be associated with the disappearance of any self-reformation process. But, this enigmatic observation reveals that 3D PIC simulation is necessary in which the*B*_{0}field is fully involved whatever its orientation is in the simulation box. Preliminary results by Shinohara et al. (2011) based on 3D PIC simulations show that both processes (emission of nonlinear whistler from the ramp and front self-reformation) can co-exist. In other words, the time variation of the ramp or foot thickness associated with the self-reformation should persist in 3D simulation; a further quantitative study is also required in order to check the scales of the corresponding front microstructures.

The numerical simulation code where the numerical results are issued from has been deposited in the archive of LATMOS laboratory at http://lembege.projet.latmos.ipsl.fr/doc3/2D_shock/ (Lembège, 2021a). It includes the sources directory (src) and the input data directory (data).

Numerical simulation results have been deposited in the archive of LATMOS laboratory at http://lembege.projet.latmos.ipsl.fr/doc3/Data_s040116_Btz/ (Lembège, 2021b). A “readme” file has been added, describing the data filenames.

CM and BL contributed to the design and implementation of the research, the analysis of the results, and the writing of the paper.

The authors declare that they have no conflict of interest.

Thanks are addressed to the International Space Science Institute (Bern, Switzerland) and the national PNST program (Le Programme National Soleil-Terre) of CNRS (Centre National de la Recherche Scientifique) for their support. Bertrand Lembege thanks IDRIS national computer center (located at Orsay, near Paris), where present results issued from numerical simulations have been obtained (DARI project A0050400295). Christian Mazelle also thanks Emmanuel Penou for providing the CL software and Karim Meziane for his help in proofreading the manuscript. The Cluster data come from the ESA archive data center: https://www.cosmos.esa.int/web/csa (last access: 12 June 2021).

This research has been supported by the Centre National d'Études Spatiales (CNES; grant nos. APR-W-EEXP/10-01-01-05 and APR-Z-ETP-E-0010/01-01-05).

This paper was edited by Elias Roussos and reviewed by two anonymous referees.

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- Abstract
- Introduction
- Motivation, data selection, and methodology
- Analysis of individual shock crossings
- Statistical analysis
- Comparison with some previous studies
- Conclusions
- Code availability
- Data availability
- Author contributions
- Competing interests
- Acknowledgements
- Financial support
- Review statement
- References

- Abstract
- Introduction
- Motivation, data selection, and methodology
- Analysis of individual shock crossings
- Statistical analysis
- Comparison with some previous studies
- Conclusions
- Code availability
- Data availability
- Author contributions
- Competing interests
- Acknowledgements
- Financial support
- Review statement
- References