Articles | Volume 40, issue 3
https://doi.org/10.5194/angeo-40-421-2022
© Author(s) 2022. 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-40-421-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Regular paper
| 
23 Jun 2022
Regular paper |
| 23 Jun 2022
| 23 Jun 2022
Estimating the impact of the 1991 Pinatubo eruption on mesospheric temperature by analyzing HALOE (UARS) temperature data
Sandra Wallis
CORRESPONDING AUTHOR
Institute of Physics, University of Greifswald, Greifswald, Germany
Christoph Gregor Hoffmann
Institute of Physics, University of Greifswald, Greifswald, Germany
Christian von Savigny
Institute of Physics, University of Greifswald, Greifswald, Germany
Related authors
Sandra Wallis, Matthew DeLand, and Christian von Savigny
Atmos. Chem. Phys., 25, 3635–3645, https://doi.org/10.5194/acp-25-3635-2025, https://doi.org/10.5194/acp-25-3635-2025, 2025
Short summary
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The 2022 Hunga Tonga – Hunga Ha'apai eruption emitted about 150 Tg H2O that partly reached the upper polar Southern Hemisphere mesosphere in the beginning of 2024. Noctilucent clouds (NLCs) did not show a clear perturbation in their occurrence frequency, but the slight increase from mid-January to February could potentially have been caused by the additional H2O. It needed 2 years to reach the summer polar mesopause region, analogous to the 1883 Krakatoa eruption that is argued to have caused the first sightings of NLCs.
Felix Wrana, Ulrike Niemeier, Larry W. Thomason, Sandra Wallis, and Christian von Savigny
Atmos. Chem. Phys., 23, 9725–9743, https://doi.org/10.5194/acp-23-9725-2023, https://doi.org/10.5194/acp-23-9725-2023, 2023
Short summary
Short summary
The stratospheric aerosol layer is a naturally occurring and permanent layer of aerosol, in this case very small droplets of mostly sulfuric acid and water, that has a cooling effect on our climate. To quantify this effect and for our general understanding of stratospheric microphysical processes, knowledge of the size of those aerosol particles is needed. Using satellite measurements and atmospheric models we show that some volcanic eruptions can lead to on average smaller aerosol sizes.
Sandra Wallis, Hauke Schmidt, and Christian von Savigny
Atmos. Chem. Phys., 23, 7001–7014, https://doi.org/10.5194/acp-23-7001-2023, https://doi.org/10.5194/acp-23-7001-2023, 2023
Short summary
Short summary
Strong volcanic eruptions are able to alter the temperature and the circulation of the middle atmosphere. This study simulates the atmospheric response to an idealized strong tropical eruption and focuses on the impact on the mesosphere. The simulations show a warming of the polar summer mesopause in the first November after the eruption. Our study indicates that this is mainly due to dynamical coupling in the summer hemisphere with a potential contribution from interhemispheric coupling.
Elizaveta Malinina, Alexei Rozanov, Ulrike Niemeier, Sandra Wallis, Carlo Arosio, Felix Wrana, Claudia Timmreck, Christian von Savigny, and John P. Burrows
Atmos. Chem. Phys., 21, 14871–14891, https://doi.org/10.5194/acp-21-14871-2021, https://doi.org/10.5194/acp-21-14871-2021, 2021
Short summary
Short summary
In the paper, changes in the stratospheric aerosol loading after the 2018 Ambae eruption were analyzed using OMPS-LP observations. The eruption was also simulated with the MAECHAM5-HAM global climate model. Generally, the model and observations agree very well. We attribute the good consistency of the results to a precisely determined altitude and mass of the volcanic injection, as well as nudging of the meteorological data. The radiative forcing from the eruption was estimated to be −0.13 W m−2.
Lukas O. Muser, Gholam Ali Hoshyaripour, Julia Bruckert, Ákos Horváth, Elizaveta Malinina, Sandra Wallis, Fred J. Prata, Alexei Rozanov, Christian von Savigny, Heike Vogel, and Bernhard Vogel
Atmos. Chem. Phys., 20, 15015–15036, https://doi.org/10.5194/acp-20-15015-2020, https://doi.org/10.5194/acp-20-15015-2020, 2020
Short summary
Short summary
Volcanic aerosols endanger aircraft and thus disrupt air travel globally. For aviation safety, it is vital to know the location and lifetime of such aerosols in the atmosphere. Here we show that the interaction of volcanic particles with each other eventually reduces their atmospheric lifetime. Moreover, we demonstrate that sunlight heats these particles, which lifts them several kilometers in the atmosphere. These findings support a more reliable forecast of volcanic aerosol dispersion.
Christian Löns, Ronald Eixmann, Christine Pohl, Alexei Rozanov, and Christian von Savigny
EGUsphere, https://doi.org/10.5194/egusphere-2025-3984, https://doi.org/10.5194/egusphere-2025-3984, 2025
This preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).
Short summary
Short summary
During the polar vortex season, so-called streamers can transport tropical air towards the pole in the middle stratosphere. This tropical air can get trapped in high-pressure areas at high latitudes after the polar vortex breaks down. In this study, remote sensing instruments are used to observe the course of such streamers by measuring the scattered solar radiation. Aerosols get transported to high latitudes at an altitude of about 25–35 km, increasing the aerosol mass there significantly.
Sandra Wallis, Matthew DeLand, and Christian von Savigny
Atmos. Chem. Phys., 25, 3635–3645, https://doi.org/10.5194/acp-25-3635-2025, https://doi.org/10.5194/acp-25-3635-2025, 2025
Short summary
Short summary
The 2022 Hunga Tonga – Hunga Ha'apai eruption emitted about 150 Tg H2O that partly reached the upper polar Southern Hemisphere mesosphere in the beginning of 2024. Noctilucent clouds (NLCs) did not show a clear perturbation in their occurrence frequency, but the slight increase from mid-January to February could potentially have been caused by the additional H2O. It needed 2 years to reach the summer polar mesopause region, analogous to the 1883 Krakatoa eruption that is argued to have caused the first sightings of NLCs.
Felix Wrana, Terry Deshler, Christian Löns, Larry W. Thomason, and Christian von Savigny
Atmos. Chem. Phys., 25, 3717–3736, https://doi.org/10.5194/acp-25-3717-2025, https://doi.org/10.5194/acp-25-3717-2025, 2025
Short summary
Short summary
There is a natural and globally occurring layer of small droplets (aerosols) at roughly 20 km altitude in the atmosphere. In this work, the size of these droplets is calculated from satellite measurements for the years 2002 to 2005, which is important for the aerosol cooling effect on Earth's climate. These years are interesting because there were no large volcanic eruptions that would change the background state of the aerosols. The results are compared to reliable balloon-borne measurements.
Anna Lange, Ulrike Niemeier, Alexei Rozanov, and Christian von Savigny
EGUsphere, https://doi.org/10.5194/egusphere-2025-1005, https://doi.org/10.5194/egusphere-2025-1005, 2025
Short summary
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Our paper investigates whether it is possible to observe injections of 1 and 2 Tg S/y (sulphur per year) into the stratosphere with the currently active satellite occultation instruments. The calculations show that, considering the natural variability and the assumptions made here, the stratospheric aerosols formed from emissions of 1 and 2 Tg S/y in the quasi steady-state phase can be detected, which is not the case in the first month of the two-year initial phase.
Christine Pohl, Felix Wrana, Alexei Rozanov, Terry Deshler, Elizaveta Malinina, Christian von Savigny, Landon A. Rieger, Adam E. Bourassa, and John P. Burrows
Atmos. Meas. Tech., 17, 4153–4181, https://doi.org/10.5194/amt-17-4153-2024, https://doi.org/10.5194/amt-17-4153-2024, 2024
Short summary
Short summary
Knowledge of stratospheric aerosol characteristics is important for understanding chemical and climate aerosol feedbacks. Two particle size distribution parameters, the aerosol extinction coefficient and the effective radius, are obtained from SCIAMACHY limb observations. The aerosol characteristics show good agreement with independent data sets from balloon-borne and satellite observations. This data set expands the limited knowledge of stratospheric aerosol characteristics.
Christian von Savigny, Anna Lange, Christoph G. Hoffmann, and Alexei Rozanov
Atmos. Chem. Phys., 24, 2415–2422, https://doi.org/10.5194/acp-24-2415-2024, https://doi.org/10.5194/acp-24-2415-2024, 2024
Short summary
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It is well known that volcanic eruptions strongly affect the colours of the twilight sky. Typically, volcanic eruptions lead to enhanced reddish and violet twilight colours. In rare cases, however, volcanic eruptions can also lead to green sunsets. This study provides an explanation for the occurrence of these unusual green sunsets based on simulations with a radiative transfer model. Green volcanic sunsets require a sufficient stratospheric aerosol optical depth and specific aerosol sizes.
Anna Lange, Alexei Rozanov, and Christian von Savigny
Atmos. Chem. Phys., 23, 14829–14839, https://doi.org/10.5194/acp-23-14829-2023, https://doi.org/10.5194/acp-23-14829-2023, 2023
Short summary
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We were able to demonstrate quantitatively that the blue colour of the sky cannot be solely attributed to Rayleigh scattering. The influence of ozone on the blue colour of the sky is calculated for different viewing geometries, total ozone columns and an enhanced stratospheric aerosol scenario. Furthermore, the effects of polarisation, surface albedo and observer height are investigated.
John M. C. Plane, Jörg Gumbel, Konstantinos S. Kalogerakis, Daniel R. Marsh, and Christian von Savigny
Atmos. Chem. Phys., 23, 13255–13282, https://doi.org/10.5194/acp-23-13255-2023, https://doi.org/10.5194/acp-23-13255-2023, 2023
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The mesosphere or lower thermosphere region of the atmosphere borders the edge of space. It is subject to extreme ultraviolet photons and charged particles from the Sun and atmospheric gravity waves from below, which tend to break in this region. The pressure is very low, which facilitates chemistry involving species in excited states, and this is also the region where cosmic dust ablates and injects various metals. The result is a unique and exotic chemistry.
Christoph G. Hoffmann, Lena G. Buth, and Christian von Savigny
Atmos. Chem. Phys., 23, 12781–12799, https://doi.org/10.5194/acp-23-12781-2023, https://doi.org/10.5194/acp-23-12781-2023, 2023
Short summary
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The Madden–Julian oscillation is an important feature of weather in the tropics. Although it is mainly active in the troposphere, we show that it systematically influences the air temperature in the layers above, up to about 100 km altitude and from pole to pole. We have linked this to another known far-reaching process, interhemispheric coupling. This is basic research on atmospheric couplings and variability but might also be of interest for intraseasonal weather forecasting models.
Felix Wrana, Ulrike Niemeier, Larry W. Thomason, Sandra Wallis, and Christian von Savigny
Atmos. Chem. Phys., 23, 9725–9743, https://doi.org/10.5194/acp-23-9725-2023, https://doi.org/10.5194/acp-23-9725-2023, 2023
Short summary
Short summary
The stratospheric aerosol layer is a naturally occurring and permanent layer of aerosol, in this case very small droplets of mostly sulfuric acid and water, that has a cooling effect on our climate. To quantify this effect and for our general understanding of stratospheric microphysical processes, knowledge of the size of those aerosol particles is needed. Using satellite measurements and atmospheric models we show that some volcanic eruptions can lead to on average smaller aerosol sizes.
Sandra Wallis, Hauke Schmidt, and Christian von Savigny
Atmos. Chem. Phys., 23, 7001–7014, https://doi.org/10.5194/acp-23-7001-2023, https://doi.org/10.5194/acp-23-7001-2023, 2023
Short summary
Short summary
Strong volcanic eruptions are able to alter the temperature and the circulation of the middle atmosphere. This study simulates the atmospheric response to an idealized strong tropical eruption and focuses on the impact on the mesosphere. The simulations show a warming of the polar summer mesopause in the first November after the eruption. Our study indicates that this is mainly due to dynamical coupling in the summer hemisphere with a potential contribution from interhemispheric coupling.
Christian von Savigny, Anna Lange, Anne Hemkendreis, Christoph G. Hoffmann, and Alexei Rozanov
Clim. Past, 18, 2345–2356, https://doi.org/10.5194/cp-18-2345-2022, https://doi.org/10.5194/cp-18-2345-2022, 2022
Short summary
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This study investigates the possibility of inferring information on aerosol optical depth from photographs of historic paintings. The idea – which has been applied in previous studies – is very interesting because it would provide an archive of the atmospheric aerosol loading covering many centuries. We show that twilight colours depend not only on the aerosol optical thickness, but also on several other parameters, making a quantitative estimate of aerosol optical depth very difficult.
Anna Lange, Gerd Baumgarten, Alexei Rozanov, and Christian von Savigny
Ann. Geophys., 40, 407–419, https://doi.org/10.5194/angeo-40-407-2022, https://doi.org/10.5194/angeo-40-407-2022, 2022
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We investigate the influence of different parameters on the colour of noctilucent clouds (highest clouds in the atmosphere), using radiative transfer calculations. We determined the effect of the particle size, optical depth, single scattering/multiple scattering and ozone. For sufficiently large optical depth and for specific viewing geometries, ozone plays only a minor role in the blueish colour of noctilucent clouds (new result).
Mireia Papke Chica, Valerian Hahn, Tiziana Braeuer, Elena de la Torre Castro, Florian Ewald, Mathias Gergely, Simon Kirschler, Luca Bugliaro Goggia, Stefanie Knobloch, Martina Kraemer, Johannes Lucke, Johanna Mayer, Raphael Maerkl, Manuel Moser, Laura Tomsche, Tina Jurkat-Witschas, Martin Zoeger, Christian von Savigny, and Christiane Voigt
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2022-255, https://doi.org/10.5194/acp-2022-255, 2022
Preprint withdrawn
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The mixed-phase temperature regime in convective clouds challenges our understanding of microphysical and radiative cloud properties. We provide a rare and unique dataset of aircraft in situ measurements in a strong mid-latitude convective system. We find that mechanisms initiating ice nucleation and growth strongly depend on temperature, relative humidity, and vertical velocity and variate within the measured system, resulting in altitude dependent changes of the cloud liquid and ice fraction.
Julia Koch, Adam Bourassa, Nick Lloyd, Chris Roth, and Christian von Savigny
Atmos. Chem. Phys., 22, 3191–3202, https://doi.org/10.5194/acp-22-3191-2022, https://doi.org/10.5194/acp-22-3191-2022, 2022
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The mesopause, the region of the earth's atmosphere between 85 and 100 km, is hard to access by direct measurements. Therefore we look for parameters that can be measured using satellite or ground-based measurements. In this study we researched sodium airglow, a phenomenon that occurs when sodium atoms are excited by chemical reactions. We compared satellite measurements of the airglow and resulting sodium concentration profiles to gain a better understanding of the sodium in that region.
Elizaveta Malinina, Alexei Rozanov, Ulrike Niemeier, Sandra Wallis, Carlo Arosio, Felix Wrana, Claudia Timmreck, Christian von Savigny, and John P. Burrows
Atmos. Chem. Phys., 21, 14871–14891, https://doi.org/10.5194/acp-21-14871-2021, https://doi.org/10.5194/acp-21-14871-2021, 2021
Short summary
Short summary
In the paper, changes in the stratospheric aerosol loading after the 2018 Ambae eruption were analyzed using OMPS-LP observations. The eruption was also simulated with the MAECHAM5-HAM global climate model. Generally, the model and observations agree very well. We attribute the good consistency of the results to a precisely determined altitude and mass of the volcanic injection, as well as nudging of the meteorological data. The radiative forcing from the eruption was estimated to be −0.13 W m−2.
Nellie Wullenweber, Anna Lange, Alexei Rozanov, and Christian von Savigny
Clim. Past, 17, 969–983, https://doi.org/10.5194/cp-17-969-2021, https://doi.org/10.5194/cp-17-969-2021, 2021
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This study investigates the physical processes leading to the rare phenomenon of the sun appearing blue or green. The phenomenon is caused by anomalous scattering by, e.g., volcanic or forest fire aerosols. Unlike most other studies, our study includes a full treatment of the effect of Rayleigh scattering on the colour of the sun. We investigate different factors and revisit a historic example, i.e. the Canadian forest fires in 1950, that led to blue sun events in different European countries.
Felix Wrana, Christian von Savigny, Jacob Zalach, and Larry W. Thomason
Atmos. Meas. Tech., 14, 2345–2357, https://doi.org/10.5194/amt-14-2345-2021, https://doi.org/10.5194/amt-14-2345-2021, 2021
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In this paper, we describe a new method for calculating the size of naturally occurring droplets (aerosols) made mostly of sulfuric acid and water that can be found roughly at 20 km altitude in the atmosphere. We use data from the instrument SAGE III/ISS that is mounted on the International Space Station. We show that our method works well, and that the size parameters we calculate are reasonable and can be a valuable addition for a better understanding of aerosols and their effect on climate.
Larry W. Thomason, Mahesh Kovilakam, Anja Schmidt, Christian von Savigny, Travis Knepp, and Landon Rieger
Atmos. Chem. Phys., 21, 1143–1158, https://doi.org/10.5194/acp-21-1143-2021, https://doi.org/10.5194/acp-21-1143-2021, 2021
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Measurements of the impact of volcanic eruptions on stratospheric aerosol loading by space-based instruments show show a fairly well-behaved relationship between the magnitude and the apparent changes to aerosol size over several orders of magnitude. This directly measured relationship provides a unique opportunity to verify the performance of interactive aerosol models used in climate models.
Lukas O. Muser, Gholam Ali Hoshyaripour, Julia Bruckert, Ákos Horváth, Elizaveta Malinina, Sandra Wallis, Fred J. Prata, Alexei Rozanov, Christian von Savigny, Heike Vogel, and Bernhard Vogel
Atmos. Chem. Phys., 20, 15015–15036, https://doi.org/10.5194/acp-20-15015-2020, https://doi.org/10.5194/acp-20-15015-2020, 2020
Short summary
Short summary
Volcanic aerosols endanger aircraft and thus disrupt air travel globally. For aviation safety, it is vital to know the location and lifetime of such aerosols in the atmosphere. Here we show that the interaction of volcanic particles with each other eventually reduces their atmospheric lifetime. Moreover, we demonstrate that sunlight heats these particles, which lifts them several kilometers in the atmosphere. These findings support a more reliable forecast of volcanic aerosol dispersion.
Cited articles
Barnes, J. E. and Hofmann, D. J.: Lidar measurements of stratospheric aerosol
over Mauna Loa Observatory, Geophys. Res. Lett., 24, 1923–1926,
https://doi.org/10.1029/97GL01943, 1997. a
Becker, E. and von Savigny, C.: Dynamical heating of the polar summer mesopause
induced by solar proton events, J. Geophys. Res.-Atmos.,
115, D00I18, https://doi.org/10.1029/2009JD012561, 2010. a
Bittner, M., Offermann, D., Graef, H.-H., Donner, M., and Hamilton, K.: An
18-year time series of OH rotational temperatures and middle atmosphere
decadal variations, J. Atmos. Sol.-Terr. Phys., 64,
1147–1166, https://doi.org/10.1016/S1364-6826(02)00065-2, 2002. a, b, c, d
Borchert, S., Zhou, G., Baldauf, M., Schmidt, H., Zängl, G., and Reinert, D.: The upper-atmosphere extension of the ICON general circulation model (version: ua-icon-1.0), Geosci. Model Dev., 12, 3541–3569, https://doi.org/10.5194/gmd-12-3541-2019, 2019. a
Efron, B.: Nonparametric Estimates of Standard Error: The Jackknife, the
Bootstrap and Other Methods, Biometrika, 68, 589–599, 1981. a
Hervig, M. E., Russell III, J. M., Gordley, L. L., Drayson, S. R., Stone, K.,
Thompson, R. E., Gelman, M. E., McDermid, I. S., Hauchecorne, A., Keckhut,
P., McGee, T. J., Singh, U. N., and Gross, M. R.: Validation of temperature
measurements from the Halogen Occultation Experiment, J. Geophys.
Res.-Atmos., 101, 10277–10285, https://doi.org/10.1029/95JD01713, 1996. a
Johnson, J.: read_haloe_l2.pro [code], https://disc.gsfc.nasa.gov/information/documents?title=UARS Mission Preservation Documents, last access: 17 June 2022. a
Kalicinsky, C., Knieling, P., Koppmann, R., Offermann, D., Steinbrecht, W., and Wintel, J.: Long-term dynamics of OH* temperatures over central Europe: trends and solar correlations, Atmos. Chem. Phys., 16, 15033–15047, https://doi.org/10.5194/acp-16-15033-2016, 2016. a, b, c
Karlsson, B., Randall, C. E., Benze, S., Mills, M., Harvey, V. L., Bailey,
S. M., and Russell III, J. M.: Intra-seasonal variability of polar
mesospheric clouds due to inter-hemispheric coupling, Geophys. Res.
Lett., 36, L20802, https://doi.org/10.1029/2009GL040348, 2009. a
Keckhut, P., Hauchecorne, A., and Chanin, M. L.: Midlatitude long-term
variability of the middle atmosphere: Trends and cyclic and episodic changes,
J. Geophys. Res.-Atmos., 100, 18887–18897,
https://doi.org/10.1029/95JD01387, 1995. a, b, c
Kerzenmacher, T. E., Keckhut, P., Hauchecorne, A., and Chanin, M.-L.:
Methodological uncertainties in multi-regression analyses of
middle-atmospheric data series, J. Environ. Monit., 8, 682–690,
https://doi.org/10.1039/B603750J, 2006. a
Kilian, M., Brinkop, S., and Jöckel, P.: Impact of the eruption of Mt Pinatubo on the chemical composition of the stratosphere, Atmos. Chem. Phys., 20, 11697–11715, https://doi.org/10.5194/acp-20-11697-2020, 2020. a
Lasp Interactive Solar Irradiance Datacenter: Penticton Solar Radio Flux at 10.7 cm, Time Series [data set], http://lasp.colorado.edu/lisird/data/penticton_radio_flux/, last access: 17 June 2022. a
Markwardt, C. B.: MPFITFUN [code], http://cow.physics.wisc.edu/~craigm/idl/down/mpfitfun.pro, last access: 17 June 2022. a
Miller, R. G.: The Jackknife – A Review, Biometrika, 61, 1–15, 1974. a
Offermann, D., Hoffmann, P., Knieling, P., Koppmann, R., Oberheide, J., and
Steinbrecht, W.: Long-term trends and solar cycle variations of mesospheric
temperature and dynamics, J. Geophys. Res.-Atmos., 115, D18127,
https://doi.org/10.1029/2009JD013363, 2010. a, b, c
Parker, D., D.E., Wilson, Jones, P., Christy, and Folland, C.: The impact of
Mount Pinatubo on world-wide temperatures, Int. J.
Climatol., 16, 487–497., 1996. a
Ramesh, K., Smith, A. K., Garcia, R. R., Marsh, D. R., Sridharan, S., and
Kishore Kumar, K.: Long‐term variability and tendencies in middle
atmosphere temperature and zonal wind from WACCM6 simulations during
1850–2014, J. Geophys. Res.-Atmos., 125, e2020JD033579, https://doi.org/10.1029/2020JD033579,
2020. a, b
Rank, G., Diehl, R., Lichti, G. G., Schönfelder, V., Varendorff, M.,
Swanenburg, B. N., van Dijk, R., Forrest, D., Macri, J., McDonnell, M.,
Loomis, M., Ryan, J., Bennett, K., and Winkler, C.: Observations of the 1991
June 11 solar flare with COMPTEL, AIP Conf. Proc., 294, 100–105,
https://doi.org/10.1063/1.45207, 1994. a
Reber, C. A., Trevathan, C. E., McNeal, R. J., and Luther, M. R.: The Upper
Atmosphere Research Satellite (UARS) mission, J. Geophys.
Res.-Atmos., 98, 10643–10647,
1993. a
Remsberg, E., Deaver, L., Wells, J., Lingenfelser, G., Bhatt, P., Gordley, L.,
Thompson, R., McHugh, M., Russell III, J. M., Keckhut, P., and Schmidlin, F.:
An assessment of the quality of Halogen Occultation Experiment temperature
profiles in the mesosphere based on comparisons with Rayleigh backscatter
lidar and inflatable falling sphere measurements, J. Geophys.
Res.-Atmos., 107, 4447, https://doi.org/10.1029/2001JD001521, 2002a. a
Remsberg, E. E.: Trends and solar cycle effects in temperature versus altitude
from the Halogen Occultation Experiment for the mesosphere and upper
stratosphere, J. Geophys. Res.-Atmos., 114, D12303,
https://doi.org/10.1029/2009JD011897, 2009. a, b, c, d
Remsberg, E. E. and Deaver, L. E.: Interannual, solar cycle, and trend terms in
middle atmospheric temperature time series from HALOE, J. Geophys.
Res.-Atmos., 110, D06106, https://doi.org/10.1029/2004JD004905, 2005. a
Remsberg, E. E., Bhatt, P. P., and Deaver, L. E.: Seasonal and longer-term
variations in middle atmosphere temperature from HALOE on UARS, J.
Geophys. Res.-Atmos., 107, 4411,
https://doi.org/10.1029/2001JD001366, 2002b. a, b
Robock, A.: Volcanic eruptions and climate, Rev. Geophys., 38,
191–219, https://doi.org/10.1029/1998RG000054, 2000. a
Russell III, J. M.: UARS Halogen Occultation Experiment (HALOE) Level 2 V019,
Greenbelt, MD, USA, Goddard Earth Sciences Data and Information Services
Center (GES DISC) [data set],
https://disc.gsfc.nasa.gov/datacollection/UARHA2FN_019.html (last access: 26 February 2020),
1999. a
Russell III, J. M., Gordley, L. L., Park, J. H., Drayson, S. R., Hesketh,
W. D., Cicerone, R. J., Tuck, A. F., Frederick, J. E., Harries, J. E., and
Crutzen, P. J.: The Halogen Occultation Experiment, J. Geophys.
Res.-Atmos., 98, 10777–10797, https://doi.org/10.1029/93JD00799, 1993. a, b
Schultz, M.: PERCENTILES [code],
https://hesperia.gsfc.nasa.gov/ssw/packages/s3drs/idl/util/percentiles.pro, last access: 17 June 2022. a
She, C.-Y., Krueger, D. A., and Yuan, T.: Long-term midlatitude mesopause region temperature trend deduced from quarter century (1990–2014) Na lidar observations, Ann. Geophys., 33, 363–369, https://doi.org/10.5194/angeo-33-363-2015, 2015. a
Smith, A. K., P. N. M., and Mullen, Z. K.: Interhemispheric Coupling Mechanisms
in the Middle Atmosphere of WACCM6, J. Atmos. Sci., 77,
1101–1118, https://doi.org/10.1175/JAS-D-19-0253.1, 2020.
a
Thompson, R. E. and Gordley, L. L.: Retrieval algorithms for the Halogen
Occultation Experiment (NASA/Contractor Report 2009-215761),
https://core.ac.uk/download/pdf/10549287.pdf (last access: 17 June 2022), 2009. a
Thulasiraman, S. and Nee, J. B.: Further evidence of a two-level mesopause and
its variations from UARS high-resolution Doppler imager temperature data,
J. Geophys. Res.-Atmos., 107, 4355,
https://doi.org/10.1029/2000JD000118, 2002. a
von Savigny, C., Timmreck, C., Buehler, S. A., Burrows, J. P., Giorgetta, M.,
Hegerl, G., Horvath, A., Hoshyaripour, G., Hoose, C., Quaas, J., Malinina,
E., Rozanov, A., Schmidt, H., Thomason, L., Toohey, M., and Vogel, B.: The
Research Unit VolImpact: Revisiting the volcanic impact on atmosphere and
climate – preparations for the next big volcanic eruption, Meteorol.
Z., 29, 3–18, 2020. a
Short summary
Although the 1991 eruption of Mt Pinatubo had a severe impact on Earth's climate, the effect of this event on the mesosphere is not well understood. We investigated satellite-borne temperature measurements from the HALOE instrument and found indications that a positive temperature anomaly is present in the tropical upper mesosphere at the beginning of the HALOE time series, which may be related to the eruption of Mt. Pinatubo.
Although the 1991 eruption of Mt Pinatubo had a severe impact on Earth's climate, the effect of...
