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@ARTICLE{Fadnavis:851443,
author = {Fadnavis, Suvarna and Roy, Chaitri and Chattopadhyay, Rajib
and Sioris, Christopher E. and Rap, Alexandru and Müller,
Rolf and Kumar, K. Ravi and Krishnan, Raghavan},
title = {{T}ransport of trace gases via eddy shedding from the
{A}sian summer monsoon anticyclone and associated impacts on
ozone heating rates},
journal = {Atmospheric chemistry and physics},
volume = {18},
number = {15},
issn = {1680-7324},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2018-05090},
pages = {11493 - 11506},
year = {2018},
abstract = {The highly vibrant Asian summer monsoon (ASM) anticyclone
plays an important role in efficient transport of Asian
tropospheric air masses to the extratropical upper
troposphere and lower stratosphere (UTLS). In this paper, we
demonstrate long-range transport of Asian trace gases via
eddy-shedding events using MIPAS (Michelson Interferometer
for Passive Atmospheric Sounding) satellite observations,
ERA-Interim reanalysis data and the ECHAM5–HAMMOZ global
chemistry-climate model. Model simulations and observations
consistently show that Asian boundary layer trace gases are
lifted to UTLS altitudes in the monsoon anticyclone and are
further transported horizontally eastward and westward by
eddies detached from the anticyclone. We present an event of
eddy shedding during 1–8 July 2003 and discuss a
1995–2016 climatology of eddy-shedding events. Our
analysis indicates that eddies detached from the anticyclone
contribute to the transport of Asian trace gases away from
the Asian region to the western Pacific (20–30°N,
120–150°E) and western Africa (20–30°N, 0–30°E).
Over the last two decades, the estimated frequency of
occurrence of eddy-shedding events is $ ∼ 68\%$
towards western Africa and $ ∼ 25\%$ towards the
western Pacific.Model sensitivity experiments considering a
$10\%$ reduction in Asian emissions of non-methane volatile
organic compounds (NMVOCs) and nitrogen oxides (NOx) were
performed with ECHAM5–HAMMOZ to understand the impact of
Asian emissions on the UTLS. The model simulations show that
transport of Asian emissions due to eddy shedding
significantly affects the chemical composition of the upper
troposphere ( ∼ 100–400hPa) and lower stratosphere
( ∼ 100–80hPa) over western Africa and the western
Pacific. The $10\%$ reduction of NMVOCs and NOx Asian
emissions leads to decreases in peroxyacetyl nitrate (PAN)
$(2\%–10\%$ near 200–80hPa), ozone $(1\%–4.5\%$ near
∼ 150hPa) and ozone heating rates
(0.001–0.004Kday−1 near 300–150hPa) in the upper
troposphere over western Africa and the western Pacific.},
cin = {IEK-7},
ddc = {550},
cid = {I:(DE-Juel1)IEK-7-20101013},
pnm = {244 - Composition and dynamics of the upper troposphere and
middle atmosphere (POF3-244)},
pid = {G:(DE-HGF)POF3-244},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000441652600005},
doi = {10.5194/acp-18-11493-2018},
url = {https://juser.fz-juelich.de/record/851443},
}