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Global perturbation of stratospheric water and aerosol burden by Hunga eruption
  • +28
  • Sergey Khaykin,
  • Aurélien Podglajen,
  • Felix Ploeger,
  • Jens-Uwe Grooß,
  • Florent Tence,
  • Slimane Bekki,
  • Konstantin Khlopenkov,
  • Kristopher Bedka,
  • Landon Rieger,
  • Alexandre Baron,
  • Sophie Godin-Beekmann,
  • Bernard Legras,
  • Pasquale Sellitto,
  • Tetsu Sakai,
  • John Barnes,
  • Osamu Uchino,
  • Isamu Morino,
  • Tomohiro Nagai,
  • Robin Wing,
  • Gerd Baumgarten,
  • Michael Gerding,
  • Valentin Duflot,
  • Guillaume Payen,
  • Julien Jumelet,
  • Richard Querel,
  • Ben Liley,
  • Adam Bourassa,
  • Alain Hauchecorne,
  • Francois Ravetta,
  • Benjamin Clouser,
  • Artem Feofilov
Sergey Khaykin
Laboratoire Atmosphère Observations Spatiales, UVSQ, CNRS, Sorbonne University, France

Corresponding Author:[email protected]

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Aurélien Podglajen
Laboratoire de Météorologie Dynamique, IPSL, CNRS, ENS-PSL/Sorbonne Univ., Paris, France
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Felix Ploeger
Forschungszentrum Jülich, Institute of Energy and Climate Research (IEK-7), Jülich, Germany
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Jens-Uwe Grooß
Forschungszentrum Jülich, Institute of Energy and Climate Research (IEK-7), Jülich, Germany
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Florent Tence
Laboratoire Atmosphère Observations Spatiales, UVSQ, CNRS, Sorbonne University, France
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Slimane Bekki
Laboratoire Atmosphère Observations Spatiales, UVSQ, CNRS, Sorbonne University, France
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Konstantin Khlopenkov
NASA Langley Research Center, Hampton, Virginia, USA
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Kristopher Bedka
NASA Langley Research Center, Hampton, Virginia, USA
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Landon Rieger
Institute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, Canada
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Alexandre Baron
Laboratoire de l’Atmosphère et des Cyclones, UMR8105, University of La Réunion, CNRS, Météo France, La Réunion, France
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Sophie Godin-Beekmann
Laboratoire Atmosphère Observations Spatiales, UVSQ, CNRS, Sorbonne University, France
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Bernard Legras
Laboratoire de Météorologie Dynamique, IPSL, CNRS, ENS-PSL/Sorbonne Univ., Paris, France
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Pasquale Sellitto
Univ. Paris Est Créteil and Université de Paris Cité, CNRS, Laboratoire Interuniversitaire des Systèmes Atmosphériques, Institut Pierre Simon Laplace, Créteil, France
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Tetsu Sakai
Meteorological Research Institute (MRI-JMA), Tsukuba, Japan
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John Barnes
NOAA Global Monitoring Laboratory, Boulder, Colorado, USA
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Osamu Uchino
National Institute for Environmental Studies (NIES), Tsukuba, Japan
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Isamu Morino
National Institute for Environmental Studies (NIES), Tsukuba, Japan
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Tomohiro Nagai
National Institute for Environmental Studies (NIES), Tsukuba, Japan
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Robin Wing
Leibniz-Institut für Atmosphärenphysik, Kühlungsborn, Germany
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Gerd Baumgarten
Leibniz-Institut für Atmosphärenphysik, Kühlungsborn, Germany
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Michael Gerding
Leibniz-Institut für Atmosphärenphysik, Kühlungsborn, Germany
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Valentin Duflot
Laboratoire de l’Atmosphère et des Cyclones, UMR8105, University of La Réunion, CNRS, Météo France, La Réunion, France
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Guillaume Payen
Observatoire des Sciences de l’Univers de la Réunion, UAR3365, University of La Réunion, La Réunion, France
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Julien Jumelet
Laboratoire Atmosphère Observations Spatiales, UVSQ, CNRS, Sorbonne University, France
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Richard Querel
National Institute of Water & Atmospheric Research (NIWA), Lauder, New Zealand
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Ben Liley
National Institute of Water & Atmospheric Research (NIWA), Lauder, New Zealand
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Adam Bourassa
Institute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, Canada
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Alain Hauchecorne
Laboratoire Atmosphère Observations Spatiales, UVSQ, CNRS, Sorbonne University, France
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Francois Ravetta
Laboratoire Atmosphère Observations Spatiales, UVSQ, CNRS, Sorbonne University, France
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Benjamin Clouser
Department of the Geophysical Sciences, University of Chicago, Chicago, IL, USA
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Artem Feofilov
LMD/IPSL, Sorbonne Université, UPMC Univ Paris 06, CNRS, École Polytechnique, Paris, France
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Abstract

The eruption of the submarine Hunga volcano in January 2022 was associated with a powerful blast that injected volcanic material to altitudes up to 58 km. From a combination of various types of satellite and ground-based observations supported by transport modeling, we show evidence for an unprecedented increase in the global stratospheric water mass by 13% as compared to climatological levels, and a 5-fold increase of stratospheric aerosol load, the highest in the last three decades. Owing to the extreme injection altitude, the volcanic plume has circumnavigated the Earth in only one week and dispersed nearly pole-to-pole in three months. The unique nature and magnitude of the global stratospheric perturbation by the Hunga eruption ranks it among the most remarkable climatic events in the modern observation era, with a range of potential persistent repercussions for stratospheric composition and climate.