Articles | Volume 17, issue 21
https://doi.org/10.5194/acp-17-13439-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-13439-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Equatorward dispersion of a high-latitude volcanic plume and its relation to the Asian summer monsoon: a case study of the Sarychev eruption in 2009
Jülich Supercomputing Centre, Forschungszentrum Jülich,
Jülich, Germany
Key Laboratory of Middle Atmosphere and Global Environment
Observation, Institute of Atmospheric Physics, Chinese Academy of Sciences,
Beijing, China
Sabine Griessbach
Jülich Supercomputing Centre, Forschungszentrum Jülich,
Jülich, Germany
Lars Hoffmann
Jülich Supercomputing Centre, Forschungszentrum Jülich,
Jülich, Germany
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- In situ measurements and backward-trajectory analysis of high-concentration, fine-mode aerosols in the UTLS over the Tibetan Plateau J. Zhang et al. 10.1088/1748-9326/ab5a9f
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Latest update: 20 Nov 2024
Short summary
This study is focused on the Sarychev eruption in 2009. Based on Lagrangian model simulations and satellite data, the equatorward transport of the plume and aerosol from the Sarychev eruption is confirmed, and the transport is facilitated by the Asian summer monsoon anticyclonic circulations. The aerosol transported to the tropics remained for months and dispersed upward, which could make the Sarychev eruption have a similar global climate impact as a tropical volcanic eruption.
This study is focused on the Sarychev eruption in 2009. Based on Lagrangian model simulations...
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