Articles | Volume 26, issue 7
https://doi.org/10.5194/acp-26-4749-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-26-4749-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Transport of volcanic aerosol from the Raikoke eruption in 2019 through the Northern Hemisphere
Institute of Climate and Energy Systems: Stratosphere (ICE-4), Forschungszentrum Jülich, Jülich, Germany
Laboratory of Middle Atmosphere and Global Environment Observation (LAGEO), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
Centre for Advanced Simulation and Analytics (CASA), Forschungszentrum Jülich, Jülich, Germany
Institute of Climate and Energy Systems: Stratosphere (ICE-4), Forschungszentrum Jülich, Jülich, Germany
Centre for Advanced Simulation and Analytics (CASA), Forschungszentrum Jülich, Jülich, Germany
Felix Plöger
Institute of Climate and Energy Systems: Stratosphere (ICE-4), Forschungszentrum Jülich, Jülich, Germany
Centre for Advanced Simulation and Analytics (CASA), Forschungszentrum Jülich, Jülich, Germany
Institute for Atmospheric and Environmental Research, University of Wuppertal, Wuppertal, Germany
Zhixuan Bai
Laboratory of Middle Atmosphere and Global Environment Observation (LAGEO), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
State Key Laboratory of Atmospheric Environment and Extreme Meteorology, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
Laboratory of Middle Atmosphere and Global Environment Observation (LAGEO), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
Sabine Griessbach
Jülich Supercomputing Centre, Forschungszentrum Jülich, Jülich, Germany
Centre for Advanced Simulation and Analytics (CASA), Forschungszentrum Jülich, Jülich, Germany
Lars Hoffmann
Jülich Supercomputing Centre, Forschungszentrum Jülich, Jülich, Germany
Centre for Advanced Simulation and Analytics (CASA), Forschungszentrum Jülich, Jülich, Germany
Frank G. Wienhold
Institute for Atmospheric and Climate Science (IAC), ETH Zurich, Zurich, Switzerland
Elizabeth Asher
Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado Boulder, Boulder, CO, USA
NOAA Global Monitoring Laboratory, Boulder, CO, USA
Alexandre A. Baron
Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado Boulder, Boulder, CO, USA
NOAA Chemical Sciences Laboratory, Boulder, CO, USA
Katie R. Smith
Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado Boulder, Boulder, CO, USA
NOAA Chemical Sciences Laboratory, Boulder, CO, USA
Troy Thornberry
NOAA Chemical Sciences Laboratory, Boulder, CO, USA
Jianchun Bian
Laboratory of Middle Atmosphere and Global Environment Observation (LAGEO), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, China
College of Atmospheric Sciences, Lanzhou University, Lanzhou, China
Michaela I. Hegglin
Institute of Climate and Energy Systems: Stratosphere (ICE-4), Forschungszentrum Jülich, Jülich, Germany
Centre for Advanced Simulation and Analytics (CASA), Forschungszentrum Jülich, Jülich, Germany
Institute for Atmospheric and Environmental Research, University of Wuppertal, Wuppertal, Germany
Department of Meteorology, University of Reading, Reading, UK
Data sets
Complete ERA5 from 1940: Fifth generation of ECMWF atmospheric reanalyses of the global climate H. Hersbach et al. https://doi.org/10.24381/cds.143582cf
TROPOMI Level 2 Sulfur Dioxide Total Column products, Version 02 Copernicus Sentinel-5P (processed by ESA) https://doi.org/10.5270/S5P-74eidii
Short summary
Balloon measurements over Lhasa, China, combined with satellite guided modelling, tracked aerosol from the 2019 Raikoke eruption through the Asian summer monsoon anticyclone. We find two altitude dependent routes into the anticyclone. It partly blocks transport but also allows entry and mixing, explaining the gradual weakening of the layers. Balloon measurements over Boulder, United States, outside the anticyclone, provide an independent check outside the region.
Balloon measurements over Lhasa, China, combined with satellite guided modelling, tracked...
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