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@ARTICLE{Matthias:842039,
author = {Matthias, Vivien and Ern, Manfred},
title = {{O}n the origin of the mesospheric quasi-stationary
planetary waves in the unusual {A}rctic winter 2015/16},
journal = {Atmospheric chemistry and physics / Discussions},
volume = {1051},
issn = {1680-7375},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2018-00323},
pages = {1 - 20},
year = {2017},
abstract = {The mid winter 2015/16 was characterized by an unusually
strong polar night jet (PNJ) and by extraordinarily large
stationary planetary wave (SPW) amplitudes in the
subtropical mesosphere. The aim of this study is to find the
origin of these mesospheric SPWs in mid winter 2015/16. The
time period studied here is split into two time periods. The
first period runs from late December 2015 until early
January 2016 and the second period from early January until
mid January 2016. 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 how
SPWs can occur in the mesosphere: 1) they propagate upward
from the stratosphere, 2) they are in situ generated by
longitudinally variable gravity wave (GW) drag, or 3) they
are in situ generated by barotropic and/or baroclinic
instabilities. Using global satellite observations from the
Microwave Limb Sounder (MLS) and from the Sounding of the
Atmosphere using Broadband Emission Radiometry (SABER) the
origin of the mesospheric SPWs is investigated for both time
periods. We found 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. At the same time we found
evidence that the mesospheric SPWs in polar latitudes were
in situ generated by longitudinally variable GW drag and
that there is a mixture of in situ generation by
longitudinally variable GW drag and by instabilities in mid
latitudes. Our results based on observations show that every
three mechanisms, upward propagating SPW and in situ
generated SPWs by longitudinally variable GW drag and
instabilities can act at the same time which confirms
earlier model studies. Additionally, a possible contribution
or impact of the unusually strong SPWs in the subtropical
mesosphere to the disruption of the 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},
doi = {10.5194/acp-2017-1051},
url = {https://juser.fz-juelich.de/record/842039},
}