Long range transport of South and East Asian anthropogenic aerosols counteracting Arctic warming ...
npj climate and atmospheric science 7(1), 101 (2024). doi:10.1038/s41612-024-00633-1 ... : The large-scale convection during the Asian summer monsoon plays an important role in the rapidtransport of boundary layer aerosols into the Asian summer monsoon anticyclone. Here, using thestate-of-the-art EC...
Main Authors: | , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Forschungzentrum Jülich
2024
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Subjects: | |
Online Access: | https://dx.doi.org/10.34734/fzj-2024-04614 https://juser.fz-juelich.de/record/1028433 |
Summary: | npj climate and atmospheric science 7(1), 101 (2024). doi:10.1038/s41612-024-00633-1 ... : The large-scale convection during the Asian summer monsoon plays an important role in the rapidtransport of boundary layer aerosols into the Asian summer monsoon anticyclone. Here, using thestate-of-the-art ECHAM6–HAMMOZ aerosol-chemistry-climate model, we show that these aerosolsare further transported to the Arctic along isentropic surfaces by the Brewer-Dobson-Circulation(BDC) during the monsoon season. Our model simulations show that East and South Asiananthropogenic emissions contribute significantly to the aerosol transported to the Arctic, whichcauses a higher negative net aerosol radiative forcing at the surface (dimming) of −0.09 ± 0.02 Wm −2and −0.07 ± 0.02 Wm −2 , respectively. Over the Arctic, the East Asian anthropogenic aerosols thatinclude large amounts of sulfate cause a seasonal mean net radiative forcing at the top of theatmosphere (TOA) of −0.003 ± 0.001Wm −2 and a surface cooling of −0.56 K while the black carbondominated aerosol from South Asia shows a positive TOA forcing of +0.004 ± ... |
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