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@ARTICLE{Han:187695,
author = {Han, X. and Hendricks-Franssen, Harrie-Jan and Rosolem, R.
and Jin, R. and Li, X. and Vereecken, H.},
title = {{C}orrection of systematic model forcing bias of {CLM}
using assimilation of cosmic-ray {N}eutrons and land surface
temperature: a study in the {H}eihe {C}atchment, {C}hina46},
journal = {Hydrology and earth system sciences},
volume = {19},
number = {1},
issn = {1607-7938},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2015-01307},
pages = {615 - 629},
year = {2015},
abstract = {The recent development of the non-invasive cosmic-ray soil
moisture sensing technique fills the gap between point-scale
soil moisture measurements and regional-scale soil moisture
measurements by remote sensing. A cosmic-ray probe measures
soil moisture for a footprint with a diameter of ~ 600 m (at
sea level) and with an effective measurement depth between
12 and 76 cm, depending on the soil humidity. In this study,
it was tested whether neutron counts also allow correcting
for a systematic error in the model forcings. A lack of
water management data often causes systematic input errors
to land surface models. Here, the assimilation procedure was
tested for an irrigated corn field (Heihe Watershed Allied
Telemetry Experimental Research – HiWATER, 2012) where no
irrigation data were available as model input although for
the area a significant amount of water was irrigated. In the
study, the measured cosmic-ray neutron counts and
Moderate-Resolution Imaging Spectroradiometer (MODIS) land
surface temperature (LST) products were jointly assimilated
into the Community Land Model (CLM) with the local ensemble
transform Kalman filter. Different data assimilation
scenarios were evaluated, with assimilation of LST and/or
cosmic-ray neutron counts, and possibly parameter estimation
of leaf area index (LAI). The results show that the direct
assimilation of cosmic-ray neutron counts can improve the
soil moisture and evapotranspiration (ET) estimation
significantly, correcting for lack of information on
irrigation amounts. The joint assimilation of neutron counts
and LST could improve further the ET estimation, but the
information content of neutron counts exceeded the one of
LST. Additional improvement was achieved by calibrating LAI,
which after calibration was also closer to independent field
measurements. It was concluded that assimilation of neutron
counts was useful for ET and soil moisture estimation even
if the model has a systematic bias like neglecting
irrigation. However, also the assimilation of LST helped to
correct the systematic model bias introduced by neglecting
irrigation and LST could be used to update soil moisture
with state augmentation.},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255) / 255 - Terrestrial Systems: From Observation to
Prediction (POF3-255)},
pid = {G:(DE-HGF)POF3-255 / G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000348929800035},
doi = {10.5194/hess-19-615-2015},
url = {https://juser.fz-juelich.de/record/187695},
}