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@ARTICLE{Yan:849791,
author = {Yan, Xiaolu and Konopka, Paul and Ploeger, Felix and Tao,
Mengchu and Müller, Rolf and Santee, Michelle L. and Bian,
Jianchun and Riese, Martin},
title = {{E}l {N}iño {S}outhern {O}scillation influence on the
{A}sian summer monsoon anticyclone},
journal = {Atmospheric chemistry and physics},
volume = {18},
number = {11},
issn = {1680-7324},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2018-03903},
pages = {8079 - 8096},
year = {2018},
abstract = {We analyse the influence of the El Niño Southern
Oscillation (ENSO) on the atmospheric circulation and the
mean ozone distribution in the tropical and subtropical UTLS
region. In particular, we focus on the impact of ENSO on the
onset of the Asian summer monsoon (ASM) anticyclone. Using
the Multivariate ENSO Index (MEI), we define climatologies
(composites) of atmospheric circulation and composition in
the months following El Niño and La Niña (boreal) winters
and investigate how ENSO-related flow anomalies propagate
into spring and summer. To quantify differences in the
divergent and non-divergent parts of the flow, the velocity
potential (VP) and the stream function (SF) are respectively
calculated from the ERA-Interim reanalysis in the vicinity
of the tropical tropopause at potential temperature level
θ = 380K. While VP quantifies the well-known ENSO
anomalies of the Walker circulation, SF can be used to study
the impact of ENSO on the formation of the ASM anticyclone,
which turns out to be slightly weaker after El Niño winters
than after La Niña winters. In addition, stratospheric
intrusions around the eastern flank of the anticyclone into
the tropical tropopause layer (TTL) are weaker in the months
after strong El Niño events due to more zonally symmetric
subtropical jets than after La Niña winters. By using
satellite (MLS) and in situ (SHADOZ) observations and model
simulations (CLaMS) of ozone, we discuss ENSO-induced
differences around the tropical tropopause. Ozone composites
show more zonally symmetric features with less in-mixed
ozone from the stratosphere into the TTL during and after
strong El Niño events and even during the formation of the
ASM anticyclone. These isentropic anomalies are overlaid
with the well-known anomalies of the faster (slower) Hadley
and Brewer–Dobson circulations after El Niño (La Niña)
winter. The duration and intensity of El Niño-related
anomalies may be reinforced through late summer and autumn
if the El Niño conditions last until the following winter.},
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:000434687100002},
doi = {10.5194/acp-18-8079-2018},
url = {https://juser.fz-juelich.de/record/849791},
}