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@ARTICLE{Schnitt:884095,
author = {Schnitt, Sabrina and Löhnert, Ulrich and Preusker, René},
title = {{P}otential of {D}ual-{F}requency {R}adar and {M}icrowave
{R}adiometer {S}ynergy for {W}ater {V}apor {P}rofiling in
the {C}loudy {T}rade-{W}ind {E}nvironment},
journal = {Journal of atmospheric and oceanic technology},
volume = {37},
number = {11},
issn = {0739-0572},
address = {Boston, Mass.},
publisher = {AMS},
reportid = {FZJ-2020-03090},
pages = {1973–1986},
year = {2020},
abstract = {High-resolution boundary-layer water vapor profile
observations are essential for understanding the interplay
between shallow convection, cloudiness and climate in the
trade wind atmosphere. As current observation techniques can
be limited by low spatial or temporal resolution, the
synergistic benefit of combining ground-based microwave
radiometer (MWR) and dual-frequency radar is investigated by
analysing the retrieval information content and uncertainty.
Synthetic MWR brightness temperatures, as well as simulated
dual wavelength ratios of two radar frequencies are
generated for a combination of Ka- and W-band (KaW), as well
as differential absorption radar (DAR) G-band frequencies
(167 and 174:8 GHz, G2). The synergy analysis is based on an
optimal estimation scheme by varying the configuration of
the observation vector. Combining MWR and KaW only
marginally increases the retrieval information content. The
synergy of MWR with G2 radar is more beneficial due to
increasing degrees of freedom (4.5), decreasing retrieval
errors, and a more realistic retrieved profile within the
cloud layer. The information and profile below and within
the cloud is driven by the radar observations, whereas the
synergistic benefit is largest above the cloud layer, where
information content is enhanced compared to a MWR-only or
DAR-only setup. For full synergistic benefits, however,
G-band radar sensitivities need to allow full-cloud
profiling; in this case, the results suggest that a combined
retrieval of MWR and G-band DAR can help close the
observational gap of current techniques.},
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},
UT = {WOS:000617313200004},
doi = {10.1175/JTECH-D-19-0110.1},
url = {https://juser.fz-juelich.de/record/884095},
}