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@ARTICLE{Krmer:884278,
author = {Krämer, Martina and Rolf, Christian and Spelten, Nicole
and Afchine, Armin and Fahey, David and Jensen, Eric and
Khaykin, Sergey and Kuhn, Thomas and Lawson, Paul and Lykov,
Alexey and Pan, Laura L. and Riese, Martin and Rollins,
Andrew and Stroh, Fred and Thornberry, Troy and Wolf,
Veronika and Woods, Sarah and Spichtinger, Peter and Quaas,
Johannes and Sourdeval, Odran},
title = {{A} {M}icrophysics {G}uide to {C}irrus – {P}art {II}:
{C}limatologies of {C}louds and {H}umidity from
{O}bservations},
journal = {Atmospheric chemistry and physics / Discussions},
volume = {},
issn = {1680-7367},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2020-03170},
pages = {2020-40},
year = {2020},
abstract = {This study presents airborne in-situ and satellite remote
sensing climatologies of cirrus clouds and humidity. The
climatologies serve as a guide to the properties of cirrus
clouds, with the new in-situ data base providing detailed
insights into boreal mid-latitudes and the tropics, while
the satellite-borne data set offers a global overview. To
this end, an extensive, quality checked data archive, the
Cirrus Guide II in-situ data base, is created from airborne
in-situ measurements during 150 flights in 24 campaigns. The
archive contains meteorological parameters, IWC, Nice, Rice,
RHice and H2O for each of the flights (IWC: ice water
content, Nice: number concentration of ice crystals, Rice:
ice crystal mean mass radius, RHice: relative humidity with
respect to ice, H2O: water vapor mixing ratio). Depending on
the specific parameter, the data base has extended by about
a factor of 5–10 compared to the previous studies of
Schiller et al. (2008), JGR, and Krämer et al. (2009), ACP.
One result of our investigations is, that across all
latitudes, the thicker liquid origin cirrus predominate at
lower altitudes, while at higher altitudes the thinner
in-situ cirrus prevail. Further, exemplary investigations of
the radiative characteristics of in-situ and liquid origin
cirrus show that the in-situ origin cirrus only slightly
warm the atmosphere, while liquid origin cirrus have a
strong cooling effect. An important step in completing the
Cirrus Guide II is the provision of the global cirrus Nice
climatology, derived by means of the retrieval algorithm
DARDAR-Nice from ten years of cirrus remote sensing
observations from satellite. The in-situ data base has been
used to evaluate and adjust the satellite observations. We
found that the global median Nice from satellite
observations is almost two times higher than the in-situ
median and increases slightly with decreasing temperature.
Nice medians of the most frequentl occuring cirrus sorted by
geographical regions are highest in the tropics, followed by
austral/boreal mid-latitudes, Antarctica and the Arctic.
Since the satellite climatologies enclose the entire spatial
and temporal Nice occurrence, we could deduce that half of
the cirrus are located in the lowest, warmest cirrus layer
and contain a significant amount of liquid origin cirrus. A
specific highlight of the study is the in-situ observations
of tropical tropopause layer (TTL) cirrus and humidity in
the Asian monsoon anticyclone and the comparison to the
surrounding tropics. In the convectively very active Asian
monsoon, peak values of Nice and IWC of 30 ppmv and 1000
ppmv are detected around the cold point tropopause (CPT).
Above the CPT, ice particles that are convectively injected
can locally add a significant amount of water available for
exchange with the stratosphere. We found IWCs of up to 8
ppmv in the Asian monsoon in comparison to only 2 ppmv in
the surrounding tropics. Also, the highest RHice inside of
the clouds as well as in clear sky (120–150 $\%)$ are
observed around and above the CPT. We attribute this to the
high amount of H2O (3–5 ppmv) in comparison to 1.5–3
ppmv in other tropical regions. The supersaturations above
the CPT suggest that the water exchange with the
stratosphere is 10–20 $\%$ higher than expected in regions
of weak convective activity and up to about 50 $\%$ in the
Asian monsoon.},
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-2020-40},
url = {https://juser.fz-juelich.de/record/884278},
}