Articles | Volume 41, issue 1
https://doi.org/10.5194/angeo-41-1-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/angeo-41-1-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The altitude of green OI 557.7 nm and blue N2+ 427.8 nm aurora
School of Physics & Astronomy, University of Southampton, Southampton, UK
Noora Partamies
Department of Arctic Geophysics, University Centre in Svalbard (UNIS), Longyearbyen, Norway
Birkeland Centre for Space Science, University of Bergen, Bergen, Norway
Björn Gustavsson
Dept. of Physics and Technology, UiT The Arctic University of Norway, Tromsø, Norway
Kirsti Kauristie
Finnish Meteorological Institute, Helsinki, Finland
Related authors
Noora Partamies, Rowan Dayton-Oxland, Katie Herlingshaw, Ilkka Virtanen, Bea Gallardo-Lacourt, Mikko Syrjäsuo, Fred Sigernes, Takanori Nishiyama, Toshi Nishimura, Mathieu Barthelemy, Anasuya Aruliah, Daniel Whiter, Lena Mielke, Maxime Grandin, Eero Karvinen, Marjan Spijkers, and Vincent E. Ledvina
Ann. Geophys., 43, 349–367, https://doi.org/10.5194/angeo-43-349-2025, https://doi.org/10.5194/angeo-43-349-2025, 2025
Short summary
Short summary
We studied the first broad band emissions, called continuum, in the dayside aurora. They are similar to Strong Thermal Emission Velocity Enhancement (STEVE) with white-, pale-pink-, or mauve-coloured light. But unlike STEVE, they follow the dayside aurora forming rays and other dynamic shapes. We used ground optical and radar observations and found evidence of heating and upwelling of both plasma and neutral air. This study provides new information on conditions for continuum emission, but its understanding will require further work.
Rowan Dayton-Oxland, Daniel K. Whiter, Hyomin Kim, and Betty Lanchester
EGUsphere, https://doi.org/10.22541/essoar.172641540.02035523/v1, https://doi.org/10.22541/essoar.172641540.02035523/v1, 2024
Short summary
Short summary
It is typically thought that the protons which precipitate down from space to cause proton aurora are accelerated by a type of plasma wave called an EMIC wave. In this study we use ground-based observations of proton aurora and Pc1 waves (the ground signature of EMIC waves) to test whether this mechanism occurs in the high Arctic over Svalbard, on the Earth's day side. We did not find any link between the proton aurora and Pc1 pulsations, contrary to our expectations.
Anton Goertz, Noora Partamies, Daniel Whiter, and Lisa Baddeley
Ann. Geophys., 41, 115–128, https://doi.org/10.5194/angeo-41-115-2023, https://doi.org/10.5194/angeo-41-115-2023, 2023
Short summary
Short summary
Poleward moving auroral forms (PMAFs) are specific types of aurora believed to be the signature of the connection of Earth's magnetic field to that of the sun. In this paper, we discuss the evolution of PMAFs with regard to their auroral morphology as observed in all-sky camera images. We interpret different aspects of this evolution in terms of the connection dynamics between the magnetic fields of Earth and the sun. This sheds more light on the magnetic interaction between the sun and Earth.
Noora Partamies, Daniel Whiter, Kirsti Kauristie, and Stefano Massetti
Ann. Geophys., 40, 605–618, https://doi.org/10.5194/angeo-40-605-2022, https://doi.org/10.5194/angeo-40-605-2022, 2022
Short summary
Short summary
We investigate the local time behaviour of auroral structures and emission height. Data are collected from the Fennoscandian Lapland and Svalbard latitutes from 7 identical auroral all-sky cameras over about 1 solar cycle. The typical peak emission height of the green aurora varies from 110 km on the nightside to about 118 km in the morning over Lapland but stays systematically higher over Svalbard. During fast solar wind, nightside emission heights are 5 km lower than during slow solar wind.
Fasil Tesema, Noora Partamies, Daniel K. Whiter, and Yasunobu Ogawa
Ann. Geophys., 40, 1–10, https://doi.org/10.5194/angeo-40-1-2022, https://doi.org/10.5194/angeo-40-1-2022, 2022
Short summary
Short summary
In this study, we present the comparison between an auroral model and EISCAT radar electron densities during pulsating aurorae. We test whether an overpassing satellite measurement of the average energy spectrum is a reasonable estimate for pulsating aurora electron precipitation. When patchy pulsating aurora is dominant in the morning sector, the overpass-averaged spectrum is found to be a reasonable estimate – but not when there is a mix of pulsating aurora types in the post-midnight sector.
Daniel K. Whiter, Hanna Sundberg, Betty S. Lanchester, Joshua Dreyer, Noora Partamies, Nickolay Ivchenko, Marco Zaccaria Di Fraia, Rosie Oliver, Amanda Serpell-Stevens, Tiffany Shaw-Diaz, and Thomas Braunersreuther
Ann. Geophys., 39, 975–989, https://doi.org/10.5194/angeo-39-975-2021, https://doi.org/10.5194/angeo-39-975-2021, 2021
Short summary
Short summary
This paper presents an analysis of high-resolution optical and radar observations of a phenomenon called fragmented aurora-like emissions (FAEs) observed close to aurora in the high Arctic. The observations suggest that FAEs are not caused by high-energy electrons or protons entering the atmosphere along Earth's magnetic field and are, therefore, not aurora. The speeds of the FAEs and their internal dynamics were measured and used to evaluate theories for how the FAEs are produced.
Joshua Dreyer, Noora Partamies, Daniel Whiter, Pål G. Ellingsen, Lisa Baddeley, and Stephan C. Buchert
Ann. Geophys., 39, 277–288, https://doi.org/10.5194/angeo-39-277-2021, https://doi.org/10.5194/angeo-39-277-2021, 2021
Short summary
Short summary
Small-scale auroral features are still being discovered and are not well understood. Where aurorae are caused by particle precipitation, the newly reported fragmented aurora-like emissions (FAEs) seem to be locally generated in the ionosphere (hence,
aurora-like). We analyse data from multiple instruments located near Longyearbyen to derive their main characteristics. They seem to occur as two types in a narrow altitude region (individually or in regularly spaced groups).
Kian Sartipzadeh, Andreas Kvammen, Björn Gustavsson, Njål Gulbrandsen, Magnar Gullikstad Johnsen, Devin Huyghebaert, and Juha Vierinen
EGUsphere, https://doi.org/10.5194/egusphere-2025-3070, https://doi.org/10.5194/egusphere-2025-3070, 2025
Short summary
Short summary
Knowing charged particle densities high above Earth is key for forecasting space weather effects on satellites and communications, but they are difficult to estimate at high latitudes because of auroras. We built an artificial intelligence model for northern Norway using radar observations, magnetic field measurements, geophysical indices and solar activity. It produces more accurate estimates than existing methods, even during auroral events, and can be adapted to other regions.
Noora Partamies, Rowan Dayton-Oxland, Katie Herlingshaw, Ilkka Virtanen, Bea Gallardo-Lacourt, Mikko Syrjäsuo, Fred Sigernes, Takanori Nishiyama, Toshi Nishimura, Mathieu Barthelemy, Anasuya Aruliah, Daniel Whiter, Lena Mielke, Maxime Grandin, Eero Karvinen, Marjan Spijkers, and Vincent E. Ledvina
Ann. Geophys., 43, 349–367, https://doi.org/10.5194/angeo-43-349-2025, https://doi.org/10.5194/angeo-43-349-2025, 2025
Short summary
Short summary
We studied the first broad band emissions, called continuum, in the dayside aurora. They are similar to Strong Thermal Emission Velocity Enhancement (STEVE) with white-, pale-pink-, or mauve-coloured light. But unlike STEVE, they follow the dayside aurora forming rays and other dynamic shapes. We used ground optical and radar observations and found evidence of heating and upwelling of both plasma and neutral air. This study provides new information on conditions for continuum emission, but its understanding will require further work.
Devin Huyghebaert, Juha Vierinen, Björn Gustavsson, Ralph Latteck, Toralf Renkwitz, Marius Zecha, Claudia C. Stephan, J. Federico Conte, Daniel Kastinen, Johan Kero, and Jorge L. Chau
EGUsphere, https://doi.org/10.5194/egusphere-2025-2323, https://doi.org/10.5194/egusphere-2025-2323, 2025
Short summary
Short summary
The phenomena of meteors occurs at altitudes of 60–120 km and can be used to measure the neutral atmosphere. We use a large high power radar system in Norway (MAARSY) to determine changes to the atmospheric density between the years of 2016–2023 at altitudes of 85–115 km. The same day-of-year is compared, minimizing changes to the measurements due to factors other than the atmosphere. This presents a novel method by which to obtain atmospheric neutral density variations.
Liisa Juusola, Ilkka Virtanen, Spencer Mark Hatch, Heikki Vanhamäki, Maxime Grandin, Noora Partamies, Urs Ganse, Ilja Honkonen, Abiyot Workayehu, Antti Kero, and Minna Palmroth
EGUsphere, https://doi.org/10.5194/egusphere-2025-2394, https://doi.org/10.5194/egusphere-2025-2394, 2025
Short summary
Short summary
Key properties of the ionospheric electrodynamics are electric fields, currents, and conductances. They provide a window to the vast and distant near-Earth space, cause Joule heating that affect satellite orbits, and drive geomagnetically induced currents (GICs) in technological conductor networks. We have developed a new method for solving the key properties of ionospheric electrodynamics from ground-based magnetic field observations.
Oliver Stalder, Björn Gustavsson, and Ilkka Virtanen
EGUsphere, https://doi.org/10.5194/egusphere-2025-2340, https://doi.org/10.5194/egusphere-2025-2340, 2025
This preprint is open for discussion and under review for Annales Geophysicae (ANGEO).
Short summary
Short summary
The rapid changes in ion composition during auroral are dynamically modeled by integrating the coupled continuity equations for 15 ionospheric species. The effect of the ionospheric variation on the inversion of ISR electron density profiles to differential energy spectra of precipitating electrons is studied. A systematic overestimation at high electron energies can be removed using a dynamic model. Comparisons are made with static and steady-state ionospheric models.
Etienne Gavazzi, Andres Spicher, Björn Gustavsson, James Clemmons, Robert Pfaff, and Douglas Rowland
EGUsphere, https://doi.org/10.5194/egusphere-2025-2098, https://doi.org/10.5194/egusphere-2025-2098, 2025
This preprint is open for discussion and under review for Annales Geophysicae (ANGEO).
Short summary
Short summary
Auroral precipitation refers to energetic particles that come down into the upper part of our atmosphere, the ionosphere. There, they collide with atoms and molecules and transfer some of their energy, causing aurora. The most rapid time-variation of this energy deposition and its consequences on the ionosphere are not fully understood. We show here that one can use a new model to study auroral precipitation on sub-second timescales and advance our understanding about small-scale dynamic aurora.
Devin Huyghebaert, Björn Gustavsson, Juha Vierinen, Andreas Kvammen, Matthew Zettergren, John Swoboda, Ilkka Virtanen, Spencer M. Hatch, and Karl M. Laundal
Ann. Geophys., 43, 99–113, https://doi.org/10.5194/angeo-43-99-2025, https://doi.org/10.5194/angeo-43-99-2025, 2025
Short summary
Short summary
The EISCAT_3D radar is a new ionospheric radar under construction in the Fennoscandia region. The radar will make measurements of plasma characteristics at altitudes above approximately 60 km. The capability of the system to make these measurements at spatial scales of less than 100 m using multiple digitised signals from each of the radar antenna panels is highlighted. There are many ionospheric small-scale processes that will be further resolved using the techniques discussed here.
Rowan Dayton-Oxland, Daniel K. Whiter, Hyomin Kim, and Betty Lanchester
EGUsphere, https://doi.org/10.22541/essoar.172641540.02035523/v1, https://doi.org/10.22541/essoar.172641540.02035523/v1, 2024
Short summary
Short summary
It is typically thought that the protons which precipitate down from space to cause proton aurora are accelerated by a type of plasma wave called an EMIC wave. In this study we use ground-based observations of proton aurora and Pc1 waves (the ground signature of EMIC waves) to test whether this mechanism occurs in the high Arctic over Svalbard, on the Earth's day side. We did not find any link between the proton aurora and Pc1 pulsations, contrary to our expectations.
Yoshimasa Tanaka, Yasunobu Ogawa, Akira Kadokura, Takehiko Aso, Björn Gustavsson, Urban Brändström, Tima Sergienko, Genta Ueno, and Satoko Saita
Ann. Geophys., 42, 179–190, https://doi.org/10.5194/angeo-42-179-2024, https://doi.org/10.5194/angeo-42-179-2024, 2024
Short summary
Short summary
We present via simulation how useful monochromatic images taken by a multi-point imager network are for auroral research in the EISCAT_3D project. We apply the generalized-aurora computed tomography (G-ACT) to modeled multiple auroral images and ionospheric electron density data. It is demonstrated that G-ACT provides better reconstruction results than the normal ACT and can interpolate ionospheric electron density at a much higher spatial resolution than observed by the EISCAT_3D radar.
Theresa Rexer, Björn Gustavsson, Juha Vierinen, Andres Spicher, Devin Ray Huyghebaert, Andreas Kvammen, Robert Gillies, and Asti Bhatt
Geosci. Instrum. Method. Data Syst. Discuss., https://doi.org/10.5194/gi-2023-18, https://doi.org/10.5194/gi-2023-18, 2024
Preprint under review for GI
Short summary
Short summary
We present a second-level calibration method for electron density measurements from multi-beam incoherent scatter radars. It is based on the well-known Flat field correction method used in imaging and photography. The methods improve data quality and useability as they account for unaccounted, and unpredictable variations in the radar system. This is valuable for studies where inter-beam calibration is important such as studies of polar cap patches, plasma irregularities and turbulence.
Thomas B. Leyser, Tima Sergienko, Urban Brändström, Björn Gustavsson, and Michael T. Rietveld
Ann. Geophys., 41, 589–600, https://doi.org/10.5194/angeo-41-589-2023, https://doi.org/10.5194/angeo-41-589-2023, 2023
Short summary
Short summary
Powerful radio waves transmitted into the ionosphere from the ground were used to study electron energization in the pumped ionospheric plasma turbulence, by detecting optical emissions from atomic oxygen. Our results obtained with the EISCAT (European Incoherent Scatter Scientific Association) facilities in northern Norway and optical detection with the ALIS (Auroral Large Imaging System) in northern Sweden suggest that long-wavelength upper hybrid waves are important in accelerating electrons.
Mizuki Fukizawa, Yoshimasa Tanaka, Yasunobu Ogawa, Keisuke Hosokawa, Tero Raita, and Kirsti Kauristie
Ann. Geophys., 41, 511–528, https://doi.org/10.5194/angeo-41-511-2023, https://doi.org/10.5194/angeo-41-511-2023, 2023
Short summary
Short summary
We use computed tomography to reconstruct the three-dimensional distributions of the Hall and Pedersen conductivities of pulsating auroras, a key research target for understanding the magnetosphere–ionosphere coupling process. It is suggested that the high-energy electron precipitation associated with pulsating auroras may have a greater impact on the closure of field-aligned currents in the ionosphere than has been previously reported.
Liisa Juusola, Ari Viljanen, Noora Partamies, Heikki Vanhamäki, Mirjam Kellinsalmi, and Simon Walker
Ann. Geophys., 41, 483–510, https://doi.org/10.5194/angeo-41-483-2023, https://doi.org/10.5194/angeo-41-483-2023, 2023
Short summary
Short summary
At times when auroras erupt on the sky, the magnetic field surrounding the Earth undergoes rapid changes. On the ground, these changes can induce harmful electric currents in technological conductor networks, such as powerlines. We have used magnetic field observations from northern Europe during 28 such events and found consistent behavior that can help to understand, and thus predict, the processes that drive auroras and geomagnetically induced currents.
Anton Goertz, Noora Partamies, Daniel Whiter, and Lisa Baddeley
Ann. Geophys., 41, 115–128, https://doi.org/10.5194/angeo-41-115-2023, https://doi.org/10.5194/angeo-41-115-2023, 2023
Short summary
Short summary
Poleward moving auroral forms (PMAFs) are specific types of aurora believed to be the signature of the connection of Earth's magnetic field to that of the sun. In this paper, we discuss the evolution of PMAFs with regard to their auroral morphology as observed in all-sky camera images. We interpret different aspects of this evolution in terms of the connection dynamics between the magnetic fields of Earth and the sun. This sheds more light on the magnetic interaction between the sun and Earth.
Johann Stamm, Juha Vierinen, Björn Gustavsson, and Andres Spicher
Ann. Geophys., 41, 55–67, https://doi.org/10.5194/angeo-41-55-2023, https://doi.org/10.5194/angeo-41-55-2023, 2023
Short summary
Short summary
The study of some ionospheric events benefit from the knowledge of how the physics varies over a volume and over time. Examples are studies of aurora or energy deposition. With EISCAT3D, measurements of ion velocity vectors in a volume will be possible for the first time. We present a technique that uses a set of such measurements to estimate electric field and neutral wind. The technique relies on adding restrictions to the estimates. We successfully consider restrictions based on physics.
Noora Partamies, Daniel Whiter, Kirsti Kauristie, and Stefano Massetti
Ann. Geophys., 40, 605–618, https://doi.org/10.5194/angeo-40-605-2022, https://doi.org/10.5194/angeo-40-605-2022, 2022
Short summary
Short summary
We investigate the local time behaviour of auroral structures and emission height. Data are collected from the Fennoscandian Lapland and Svalbard latitutes from 7 identical auroral all-sky cameras over about 1 solar cycle. The typical peak emission height of the green aurora varies from 110 km on the nightside to about 118 km in the morning over Lapland but stays systematically higher over Svalbard. During fast solar wind, nightside emission heights are 5 km lower than during slow solar wind.
Mizuki Fukizawa, Takeshi Sakanoi, Yoshimasa Tanaka, Yasunobu Ogawa, Keisuke Hosokawa, Björn Gustavsson, Kirsti Kauristie, Alexander Kozlovsky, Tero Raita, Urban Brändström, and Tima Sergienko
Ann. Geophys., 40, 475–484, https://doi.org/10.5194/angeo-40-475-2022, https://doi.org/10.5194/angeo-40-475-2022, 2022
Short summary
Short summary
The pulsating auroral generation mechanism has been investigated by observing precipitating electrons using rockets or satellites. However, it is difficult for such observations to distinguish temporal changes from spatial ones. In this study, we reconstructed the horizontal 2-D distribution of precipitating electrons using only auroral images. The 3-D aurora structure was also reconstructed. We found that there were both spatial and temporal changes in the precipitating electron energy.
Sebastian Käki, Ari Viljanen, Liisa Juusola, and Kirsti Kauristie
Ann. Geophys., 40, 107–119, https://doi.org/10.5194/angeo-40-107-2022, https://doi.org/10.5194/angeo-40-107-2022, 2022
Short summary
Short summary
During auroral substorms, the ionospheric electric currents change rapidly, and a large amount of energy is dissipated. We combine ionospheric current data derived from the Swarm satellite mission with the substorm database from the SuperMAG ground magnetometer network. We obtain statistics of the strength and location of the currents relative to the substorm onset. Our results show that low-earth orbit satellites give a coherent picture of the main features in the substorm current system.
Derek McKay, Juha Vierinen, Antti Kero, and Noora Partamies
Geosci. Instrum. Method. Data Syst., 11, 25–35, https://doi.org/10.5194/gi-11-25-2022, https://doi.org/10.5194/gi-11-25-2022, 2022
Short summary
Short summary
When radio waves from our galaxy enter the Earth's atmosphere, they are absorbed by electrons in the upper atmosphere. It was thought that by measuring the amount of absorption, it would allow the height of these electrons in the atmosphere to be determined. If so, this would have significance for future instrument design. However, this paper demonstrates that it is not possible to do this, but it does explain how multiple-frequency measurements can nevertheless be useful.
Fasil Tesema, Noora Partamies, Daniel K. Whiter, and Yasunobu Ogawa
Ann. Geophys., 40, 1–10, https://doi.org/10.5194/angeo-40-1-2022, https://doi.org/10.5194/angeo-40-1-2022, 2022
Short summary
Short summary
In this study, we present the comparison between an auroral model and EISCAT radar electron densities during pulsating aurorae. We test whether an overpassing satellite measurement of the average energy spectrum is a reasonable estimate for pulsating aurora electron precipitation. When patchy pulsating aurora is dominant in the morning sector, the overpass-averaged spectrum is found to be a reasonable estimate – but not when there is a mix of pulsating aurora types in the post-midnight sector.
Daniel K. Whiter, Hanna Sundberg, Betty S. Lanchester, Joshua Dreyer, Noora Partamies, Nickolay Ivchenko, Marco Zaccaria Di Fraia, Rosie Oliver, Amanda Serpell-Stevens, Tiffany Shaw-Diaz, and Thomas Braunersreuther
Ann. Geophys., 39, 975–989, https://doi.org/10.5194/angeo-39-975-2021, https://doi.org/10.5194/angeo-39-975-2021, 2021
Short summary
Short summary
This paper presents an analysis of high-resolution optical and radar observations of a phenomenon called fragmented aurora-like emissions (FAEs) observed close to aurora in the high Arctic. The observations suggest that FAEs are not caused by high-energy electrons or protons entering the atmosphere along Earth's magnetic field and are, therefore, not aurora. The speeds of the FAEs and their internal dynamics were measured and used to evaluate theories for how the FAEs are produced.
Johann Stamm, Juha Vierinen, and Björn Gustavsson
Ann. Geophys., 39, 961–974, https://doi.org/10.5194/angeo-39-961-2021, https://doi.org/10.5194/angeo-39-961-2021, 2021
Short summary
Short summary
Measurements of the electric field and neutral wind in the ionosphere are important for understanding energy flows or electric currents. With incoherent scatter radars (ISRs), we can measure the velocity of the ions, which depends on both the electrical field and the neutral wind. In this paper, we investigate methods to use ISR data to find reasonable values for both parameters. We find that electric field can be well measured down to 125 km height and neutral wind below this height.
Florine Enengl, Noora Partamies, Nickolay Ivchenko, and Lisa Baddeley
Ann. Geophys., 39, 795–809, https://doi.org/10.5194/angeo-39-795-2021, https://doi.org/10.5194/angeo-39-795-2021, 2021
Short summary
Short summary
Energetic particle precipitation has the potential to change the neutral atmospheric temperature at the bottom of the ionosphere. We have searched for events and investigated a possible correlation between lower-ionosphere electron density enhancements and simultaneous neutral temperature changes. Six of the 10 analysed events are associated with a temperature decrease of 10–20K. The events change the chemical composition in the mesosphere, and the temperatures are probed at lower altitudes.
Torbjørn Tveito, Juha Vierinen, Björn Gustavsson, and Viswanathan Lakshmi Narayanan
Ann. Geophys., 39, 427–438, https://doi.org/10.5194/angeo-39-427-2021, https://doi.org/10.5194/angeo-39-427-2021, 2021
Short summary
Short summary
This work explores the role of EISCAT 3D as a tool for planetary mapping. Due to the challenges inherent in detecting the signals reflected from faraway bodies, we have concluded that only the Moon is a viable mapping target. We estimate the impact of the ionosphere on lunar mapping, concluding that its distorting effects should be easily manageable. EISCAT 3D will be useful for mapping the lunar nearside due to its previously unused frequency (233 MHz) and its interferometric capabilities.
Joshua Dreyer, Noora Partamies, Daniel Whiter, Pål G. Ellingsen, Lisa Baddeley, and Stephan C. Buchert
Ann. Geophys., 39, 277–288, https://doi.org/10.5194/angeo-39-277-2021, https://doi.org/10.5194/angeo-39-277-2021, 2021
Short summary
Short summary
Small-scale auroral features are still being discovered and are not well understood. Where aurorae are caused by particle precipitation, the newly reported fragmented aurora-like emissions (FAEs) seem to be locally generated in the ionosphere (hence,
aurora-like). We analyse data from multiple instruments located near Longyearbyen to derive their main characteristics. They seem to occur as two types in a narrow altitude region (individually or in regularly spaced groups).
Johann Stamm, Juha Vierinen, Juan M. Urco, Björn Gustavsson, and Jorge L. Chau
Ann. Geophys., 39, 119–134, https://doi.org/10.5194/angeo-39-119-2021, https://doi.org/10.5194/angeo-39-119-2021, 2021
Cited articles
Abreu, V. J., Solomon, S. C., Sharp, W. E., and Hays, P. B.: The dissociative
recombination of O : The quantum yield of O(1S) and
O(1D), J. Geophys. Res., 88, 4140–4144,
https://doi.org/10.1029/JA088iA05p04140, 1983. a
Alge, E., Adams, N. G., and Smith, D.: Measurements of the dissociative
recombination coefficients of O , NO+ and NH in the
temperature range 200–600K, J. Phys. B, 16, 1433–1444,
https://doi.org/10.1088/0022-3700/16/8/017, 1983. a
Barth, C. A.: Nitric oxide in the lower thermosphere, Planet. Space Sci., 40,
315–336, https://doi.org/10.1016/0032-0633(92)90067-X, 1992. a
Bates, D. R.: The emission of the negative system of nitrogen from the upper
atmosphere and the significance of the twilight flash in the theory of the
ionosphere, Proc. R. Soc. Lond. A, 196, 562–591,
https://doi.org/10.1098/rspa.1949.0046, 1949. a
Billett, D. D., McWilliams, K. A., and Conde, M. G.: Colocated Observations
of the E and F Region Thermosphere During a Substorm, J. Geophys. Res.,
125, e2020JA028165, https://doi.org/10.1029/2020JA028165, 2020. a
Boyd, J. S., Belon, A. E., and Romick, G. J.: Latitude and Time Variations in
Precipitated Electron Energy Inferred from Measurements of Auroral Heights,
J. Geophys. Res., 76, 7694–7700, 1971. a
Broadfoot, A. L.: Resonance scattering by N , Planet. Space Sci., 15,
1801–1815, https://doi.org/10.1016/0032-0633(67)90017-7, 1967. a
Burns, G. B. and Reid, J. S.: Impulse response analysis of 5577Å emissions,
Planet. Space Sci., 32, 515–523, https://doi.org/10.1016/0032-0633(84)90130-2, 1984. a
Emmert, J. T., Drob, D. P., Picone, J. M., Siskind, D. E., Jones Jr., M.,
Mlynczak, M. G., Bernath, P. F., Chu, X., Doornbos, E., Funke, B.,
Goncharenko, L. P., Hervig, M. E., Schwartz, M. J., Sheese, P. E., Vargas,
F., Williams, B. P., and Yuan, T.: NRLMSIS 2.0: A Whole-Atmosphere
Empirical Model of Temperature and Neutral Species Densities, Earth Space
Sci., 8, e01321, https://doi.org/10.1029/2020EA001321, 2021. a, b
Finnish Meteorological Institute: MIRACLE All-Sky Cameras [data set],
https://space.fmi.fi/MIRACLE/ASC/, last access: 21 December 2022. a
Fox, J. L. and Hać, A. B.: Escape of O(3P), O(1D), and O(1S)
from the Martian atmosphere, Icarus, 300, 411–439,
https://doi.org/10.1016/j.icarus.2017.08.041, 2018. a
Gattinger, R. L., Harris, F. R., and Vallance Jones, A.: The height, spectrum
and mechanism of type-B red aurora and its bearing on the excitation of
O(1S) in aurora, Planet. Space Sci., 33, 201–221,
https://doi.org/10.1016/0032-0633(85)90131-X, 1985. a
Gattinger, R. L., Llewellyn, E. J., and Vallance Jones, A.: On I(5577 Å)
and I(7620 Å) auroral emissions and atomic oxygen densities, Ann.
Geophys., 14, 687–698, https://doi.org/10.1007/s00585-996-0687-1, 1996. a, b, c
Gerdjikova, M. G. and Shepherd, G. G.: Evaluation of auroral 5577-Å
excitation processes using Intercosmos Bulgaria 1300 satellite
measurements, J. Geophys. Res., 92, 3367–3374,
https://doi.org/10.1029/JA092iA04p03367, 1987. a
Gilmore, F. R., Laher, R. R., and Espy, P. J.: Franck-Condon Factors,
r-Centroids, Electronic Transition Moments, and Einstein Coefficients for
Many Nitrogen and Oxygen Band Systems, J. Phys. Chem. Ref. Data, 21,
1005–1107, https://doi.org/10.1063/1.555910, 1992. a
Green, A. E. S. and Stolarski, R. S.: Analytic models of electron impact
excitation cross sections, J. Atmos. Terr. Phys., 34, 1703–1717,
https://doi.org/10.1016/0021-9169(72)90030-X, 1972. a
Griffin, E., Kosch, M., Aruliah, A., Kavanagh, A., McWhirter, I., Senior, A.,
Ford, E., Davis, C., Abe, T., Kurihara, J., Kauristie, K., and Ogawa, Y.:
Combined ground-based optical support for the aurora (DELTA) sounding
rocket campaign, Earth Planet. Space, 58, 1113–1121,
https://doi.org/10.1186/BF03352000, 2006. a
Harang, L.: The Aurorae, Chapman & Hall, London, 1951. a
Henriksen, K.: Photometric investigation of the 4278 Å and 5577 Å
emissions in aurora, J. Atmos. Terr. Phys., 35, 1341–1350,
https://doi.org/10.1016/0021-9169(73)90167-0, 1973. a
Henriksen, K. and Egeland, A.: The Interpretation of the Auroral Green Line,
Eos Trans. AGU, 69, 721–734, https://doi.org/10.1029/88EO01015, 1988. a
Hill, S. M., Solomon, S. C., Cleary, D. D., and Broadfoot, A. L.: Temperature
dependence of the reaction N2(A )+O in the terrestrial
thermosphere, J. Geophys. Res., 105, 10615–10630,
https://doi.org/10.1029/1999JA000395, 2000. a, b
Itikawa, Y.: Cross sections for electron collisions with nitrogen molecules, J.
Phys. Chem. Ref. Data, 35, 31–53, https://doi.org/10.1063/1.1937426, 2006. a
Jokiaho, O., Lanchester, B. S., and Ivchenko, N.: Resonance scattering by
auroral N : steady state theory and observations from Svalbard, Ann.
Geophys., 27, 3465–3478, https://doi.org/10.5194/angeo-27-3465-2009, 2009. a
Kaila, K. U.: Determination of the energy of auroral electrons by the
measurements of the emission ratio and altitude of aurorae, Planet. Space
Sci., 37, 341–349, 1989. a
Kalmoni, N. M. E., Rae, I. J., Murphy, K. R., Forsyth, C., Watt, C. E. J., and
Owen, C. J.: Statistical azimuthal structuring of the substorm onset arc:
Implications for the onset mechanism, Geophys. Res. Lett., 44, 2078–2087,
https://doi.org/10.1002/2016GL071826, 2017. a
Kauristie, K., Pulkkinen, T. I., Pellinen, R. J., and Opgenoorth, H. J.: What
can we tell about global auroral-electrojet activity from a single meridional
magnetometer chain?, Ann. Geophys., 14, 1177–1185,
https://doi.org/10.1007/s00585-996-1177-1, 1996. a
Kella, D., Vejby-Christensen, L., Johnson, P. J., Pedersen, H. B., and
Andersen, L. H.: The Source of Green Light Emission Determined from a
Heavy-Ion Storage Ring Experiment, Science, 276, 1530–1533,
https://doi.org/10.1126/science.276.5318.1530, 1997. a, b, c
Knudsen, D. J., Donovan, E. F., Cogger, L. L., Jackel, B., and Shaw, W. D.:
Width and structure of mesoscale optical auroral arcs, Geophys. Res. Lett.,
28, 705–708, 2001. a
Kosch, M. J., Yiu, I., Anderson, C., Tsuda, T., Ogawa, Y., Nozawa, S., Aruliah,
A., Howells, V., Baddeley, L. J., McCrea, I. W., and Wild, J. A.: Mesoscale
observations of Joule heating near an auroral arc and ion-neutral collision
frequency in the polar cap E region, J. Geophys. Res., 116, A05321,
https://doi.org/10.1029/2010JA016015, 2011. a
Lanchester, B. and Gustavsson, B.: Imaging of Aurora to Estimate the Energy and
Flux of Electron Precipitation, Vol. 197 of Geophysical Monograph Series, 171–182, American Geophysical Union (AGU),
https://doi.org/10.1029/2011GM001161, 2012. a
Lanchester, B. S., Rees, M. H., Lummerzheim, D., Otto, A.,
Sedgemore-Schulthess, K. J. F., Zhu, H., and McCrea, I. W.: Ohmic heating as
evidence for strong field-aligned currents in filamentary aurora, J. Geophys.
Res., 106, 1785–1794, https://doi.org/10.1029/1999JA000292, 2001. a
LeClair, L. R. and McConkey, J. W.: Selective detection of O(1S0)
following electron impact dissociation of O2 and N2O using a
XeO* conversion technique, J. Chem. Phys., 99, 4566,
https://doi.org/10.1063/1.466056, 1993. a
Lin, C. and Kaufman, F.: Reactions of Metastable Nitrogen Atoms, J. Chem.
Phys., 55, 3760–3770, https://doi.org/10.1063/1.1676660, 1971. a
Lummerzheim, D. and Lilensten, J.: Electron transport and energy degradation in
the ionosphere: evaluation of the numerical solution comparison with
laboratory experiments and auroral observations, Ann. Geophys., 12,
1039–1051, 1994. a
Matzka, J., Bronkalla, O., Tornow, K., Elger, K., and Stolle, C.: GFZ Data
Services: Geomagnetic Kp index, V. 1.0 [data set], https://doi.org/10.5880/Kp.0001, 2022. a
Mehr, F. J. and Biondi, M. A.: Electron Temperature Dependence of Recombination
of O and N Ions with Electrons, Phys. Rev., 181, 264–271,
https://doi.org/10.1103/PhysRev.181.264, 1969. a
O'Neil, R. R., Lee, E. T. P., and Huppi, E. R.: Auroral O(1S) production
and loss processes: Ground-based measurements of the artificial auroral
experiment Precede, J. Geophys. Res., 84, 823–833,
https://doi.org/10.1029/JA084iA03p00823, 1979. a
Partamies, N., Whiter, D., Kauristie, K., and Massetti, S.: Local time
dependence of auroral peak emission height and morphology, Ann. Geophys., 40,
605–618, https://doi.org/10.5194/angeo-40-605-2022, 2022. a, b
Petrignani, A., van der Zande, W. J., Cosby, P. C., Hellberg, F., Thomas,
R. D., and Larsson, M.: Vibrationally resolved rate coefficients and
branching fractions in the dissociative recombination of O , J. Chem.
Phys., 122, 014302, https://doi.org/10.1063/1.1825991, 2005. a
Peverall, R., Rosén, S., Peterson, J. R., Larsson, M., Al-Khalili, A.,
Vikor, L., Semaniak, J., Bobbenkamp, R., Le Padellec, A., Maurellis, A. N.,
and van der Zande, W. J.: Dissociative recombination and excitation of
O : Cross sections, product yields and implications for studies of
ionospheric airglows, J. Chem. Phys., 114, 6679–6689,
https://doi.org/10.1063/1.1349079, 2001. a
Piper, L. G.: The excitation of O(1S) in the reaction between
N2( ) and O(3P), J. Chem. Phys., 77, 2373–2377,
https://doi.org/10.1063/1.444158, 1982. a, b, c, d
Piper, L. G.: Reevaluation of the transition-moment function and Einstein
coefficients for the N2(A –X ) transition, J.
Chem. Phys., 99, 3174–3181, https://doi.org/10.1063/1.465178, 1993. a
Sharp, W. E. and Torr, D. G.: Determination of the auroral O(1S)
production sources from coordinated rocket and satellite measurements, J.
Geophys. Res., 84, 5345–5349, https://doi.org/10.1029/JA084iA09p05345, 1979. a
Sheehan, C. H. and St.-Maurice, J.-P.: Dissociative recombination of
N , O , and NO+: Rate coefficients for ground state and
vibrationally excited ions, J. Geophys. Res., 109, A03302,
https://doi.org/10.1029/2003JA010132, 2004. a, b
Space Weather Canada: Solar radio flux – archive of measurements [data set],
https://spaceweather.gc.ca/forecast-prevision/solar-solaire/solarflux/sx-5-en.php, last access: 21
December 2022.
a
Störmer, C.: Altitudes of Auroræ, Nature, 97, 5, https://doi.org/10.1038/097005b0, 1916. a
Störmer, C.: The Polar Aurora, The Clarendon Press, Oxford, 1955. a
Strickland, D. J., Jr., R. E. D., Jasperse, J. R., and Basu, B.:
Transport-theoretic model for the electron-proton-hydrogen atom aurora: 2.
Model results, J. Geophys. Res., 98, 21533–21548,
https://doi.org/10.1029/93JA01645, 1993. a
Syrjäsuo, M., Pulkkinen, T. I., Janhunen, P., Viljanen, A., Pellinen,
R. J., Kauristie, K., Opgenoorth, H. J., Wallman, S., Eglitis, P., Karlsson,
P., Amm, O., Nielsen, E., and Thomas, C.: Observations of Substorm
Electrodynamics Using the MIRACLE Network, in: Proceedings of the
International Conference on Substorms-4, Lake Hamana, Japan, March 9–13,
edited by: Kokubun, S. and Kamide, Y., 111–114, Terra Scientific
Publishing, Tokyo, Japan, ISBN: 9780792354659, 1998. a
Tanaka, Y.-M., Kubota, M., Ishii, M., Monzen, Y., Murayama, Y., Mori, H., and
Lummerzheim, D.: Spectral type of auroral precipitating electrons estimated
from optical and cosmic noise absorption measurements, J. Geophys. Res., 111,
A11207, https://doi.org/10.1029/2006JA011744, 2006. a
Thomas, J. M. and Kaufman, F.: Rate constants of the reactions of metastable
N2(A ) in , and 3 with ground state O2 and
O, J. Chem. Phys., 83, 2900–2903, https://doi.org/10.1063/1.449243, 1985. a
Valk, F., Aints, M., Paris, P., Plank, T., Maksimov, J., and Tamm, A.:
Measurement of collisional quenching rate of nitrogen states
N2(C3Πu, v=0) and N ( , v=0), J. Phys. D:
Appl. Phys., 43, 385202, https://doi.org/10.1088/0022-3727/43/38/385202, 2010. a
Vallance Jones, A. and Gattinger, R. L.: Vibrational development and quenching
effects in the N2 (B3Πg– ) and N
(A2Πu–X2Σg) systems in aurora, J. Geophys. Res., 83,
3255–3261, https://doi.org/10.1029/JA083iA07p03255, 1978. a
Whiter, D. K., Lanchester, B. S., Sakanoi, T., and Asamura, K.: Estimating
high-energy electron fluxes by intercalibrating Reimei optical and particle
measurements using an ionospheric model, J. Atmos. Sol.-Terr. Phys., 89,
8–17, https://doi.org/10.1016/J.JASTP.2012.06.014, 2012. a
Whiter, D. K., Gustavsson, B., Partamies, N., and Sangalli, L.: A new automatic
method for estimating the peak auroral emission height from all-sky camera
images, Geosci. Instrum. Method. Data Syst., 2, 131–144,
https://doi.org/10.5194/gi-2-131-2013, 2013. a, b, c, d
Wiese, W. L., Fuhr, J. R., and Deters, T. M.: Atomic transition probabilities
of carbon, nitrogen, and oxygen – A critical data compilation, J. Phys.
Chem. Ref. Data, Monograph No. 7, AIP Press, Melville, New York, ISBN: 9781563966026, 1996. a
Yonker, J. D. and Bailey, S. M.: N2(A) in the Terrestrial Thermosphere, J.
Geophys. Res., 125, e2019JA026508, https://doi.org/10.1029/2019JA026508, 2020. a, b, c
Short summary
We measured the height of green and blue aurorae using thousands of camera images recorded over a 7-year period. Both colours are typically brightest at about 114 km altitude. When they peak at higher altitudes the blue aurora is usually higher than the green aurora. This information will help other studies which need an estimate of the auroral height. We used a computer model to explain our observations and to investigate how the green aurora is produced.
We measured the height of green and blue aurorae using thousands of camera images recorded over...