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@ARTICLE{Reutter:866945,
author = {Reutter, P. and Neis, Patrick and Rohs, Susanne and
Sauvage, B.},
title = {{C}omparison of {IAGOS} in-situ water vapour measurements
and {ECMWF} {ERA}-{I}nterim {R}eanalysis data},
journal = {Atmospheric chemistry and physics / Discussions},
volume = {573},
issn = {1680-7367},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2019-05992},
pages = {},
year = {2019},
abstract = {Abstract. Cirrus clouds and their potential formation
regions, so-called ice-supersaturated regions (ISSRs) occur
frequently in the tropopause region. It is assumed that
ISSRs and cirrus clouds can change the tropopause structure
by diabatic processes, driven by latent heating due to phase
transition and interaction with radiation. For many research
questions a three-dimensional picture including a sufficient
temporal resolution of the water vapour fields in the
tropopause region is required. This requirement is fulfilled
nowadays by reanalysis products such as the European Centre
for Medium-Range Weather Forecasts (ECMWF) ERA-Interim
reanalysis. However, for a meaningful investigation of water
vapour in the tropopause region a comparison of the
reanalysis data with measurement is advisable, since it is
difficult to measure water vapour and to assimilate
meaningful measurements into reanalysis products. Here, we
present an intercomparison of high-resolution in-situ
measurements aboard passenger aircraft within the European
Research Infrastructure IAGOS (In-service Aircraft for a
Global Observing System; http://www.iagos.org) with
ERA-Interim. Temperature and humidity data over the North
Atlantic from 2000 to 2010 are compared relative to the
dynamical tropopause. The comparison of the temperature
shows a good agreement between measurement and ERA-Interim.
While ERA-Interim can reproduce the main features of the
water vapour measurements of IAGOS, the variability of the
data is underestimated by the reanalysis data. The
combination of temperature and water vapour leads to the
relative humidity with respect to ice (RHi). Here
ERA-Interim deviates from the measurements concerning values
of larger than RHi=100 $\%,$ both in number and strength of
supersaturation. The comparison of ISSR pathlengths shows
distinct differences, which can be traced back to the
spatial resolution of both data sets. IAGOS shows
significantly more smaller ISSRs compared to ERA-Interim. A
good agreement begins only at pathlengths in the order of
the ERA-Interim spatial resolution and larger.},
cin = {IEK-8},
ddc = {550},
cid = {I:(DE-Juel1)IEK-8-20101013},
pnm = {243 - Tropospheric trace substances and their
transformation processes (POF3-243)},
pid = {G:(DE-HGF)POF3-243},
typ = {PUB:(DE-HGF)16},
doi = {10.5194/acp-2019-573},
url = {https://juser.fz-juelich.de/record/866945},
}