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@ARTICLE{Matthias:857909,
author = {Matthias, Vivien and Ern, Manfred},
title = {{O}n the origin of the mesospheric quasi-stationary
planetary waves in the unusual {A}rctic winter 2015/2016},
journal = {Atmospheric chemistry and physics},
volume = {18},
number = {7},
issn = {1680-7324},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2018-06863},
pages = {4803 - 4815},
year = {2018},
abstract = {The midwinter 2015/2016 was characterized by an unusually
strong polar night jet (PNJ) and extraordinarily large
stationary planetary wave (SPW) amplitudes in the
subtropical mesosphere. The aim of this study is, therefore,
to find the origin of these mesospheric SPWs in the
midwinter 2015/2016 study period. The study duration is
split into two periods: the first period runs from late
December 2015 until early January 2016 (Period I), and the
second period from early January until mid-January 2016
(Period II). While the SPW 1 dominates in the subtropical
mesosphere in Period I, it is the SPW 2 that dominates in
Period II. There are three possibilities explaining how SPWs
can occur in the mesosphere: (1) they propagate upward from
the stratosphere, (2) they are generated in situ by
longitudinally variable gravity wave (GW) drag, or (3) they
are generated in situ by barotropic and/or baroclinic
instabilities. Using global satellite observations from the
Microwave Limb Sounder (MLS) and the Sounding of the
Atmosphere using Broadband Emission Radiometry (SABER) the
origin of the mesospheric SPWs is investigated for both time
periods. We find that due to the strong PNJ the SPWs were
not able to propagate upward into the mesosphere northward
of 50°N but were deflected upward and equatorward into the
subtropical mesosphere. We show that the SPWs observed in
the subtropical mesosphere are the same SPWs as in the
mid-latitudinal stratosphere. Simultaneously, we find
evidence that the mesospheric SPWs in polar latitudes were
generated in situ by longitudinally variable GW drag and
that there is a mixture of in situ generation by
longitudinally variable GW drag and by instabilities at
mid-latitudes. Our results, based on observations, show that
the abovementioned three mechanisms can act at the same time
which confirms earlier model studies. Additionally, the
possible contribution from, or impact of, unusually strong
SPWs in the subtropical mesosphere to the disruption of the
quasi-biennial oscillation (QBO) in the same winter is
discussed.},
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:000429473600005},
doi = {10.5194/acp-18-4803-2018},
url = {https://juser.fz-juelich.de/record/857909},
}