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@ARTICLE{Liu:904464,
author = {Liu, Jin and Chai, Linna and Dong, Jianzhi and Zheng,
Donghai and Wigneron, J.-P. and Liu, Shaomin and Zhou, Ji
and Xu, Tongren and Yang, Shiqi and Song, Yongze and Qu,
Yuquan and Lu, Zheng},
title = {{U}ncertainty analysis of eleven multisource soil moisture
products in the third pole environment based on the
three-corned hat method},
journal = {Remote sensing of environment},
volume = {255},
issn = {0034-4257},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2021-06034},
pages = {112225 -},
year = {2021},
note = {Ein Postprint steht leider nicht zur Verfügung},
abstract = {Soil moisture (SM) is a fundamental environmental variable
for characterizing climate, land surface and atmosphere. In
recent years, several SM products have been developed based
on remote sensing (RS), land surface model (LSM) or land
data assimilation system (LDAS). However, little knowledge
is available in understanding spatial patterns of the
uncertainty of different SM products and potential regional
drivers over the Qinghai-Tibet Plateau (QTP), a complex
environment for accurate SM estimation. This paper
investigates the sensitivity of the SM uncertainties based
on the three-cornered hat (TCH) method and a generalized
additive model (GAM) in terms of underlying surface
characteristics (sand fraction, soil organic matter,
vegetation, land surface temperature, and topography) and
near-ground meteorology (precipitation and air temperature)
in the third pole environment over the 2015–2018 period.
Eleven SM products are involved in this work, including Soil
Moisture Active Passive (SMAP), Soil Moisture Ocean Salinity
INRA-CESBIO (SMOS-IC), Japan Aerospace Exploration Agency
(JAXA), Land Surface Parameter Model (LPRM), Climate Change
Initiative - Active/Combined $(CCI_A/CCI_C),$ Global Land
Data Assimilation System (GLDAS), European Centre for
Medium-Range Weather Forecasts Interim reanalysis
(ERA-Interim), Global Land Evaporation Amsterdam Model
product a/b $(GLEAM_a/GLEAM_b),$ and Random Forest Soil
Moisture (RFSM). Results show that most of the SM products
perform well across QTP, while SMOS-IC is strongly affected
by radio-frequency interference in this region, JAXA has a
relatively higher noise level over QTP, and LPRM has larger
relative uncertainties (RUs) in the southeast of QTP.
Nonlinear regression analysis demonstrates that variations
of RUs in SMOS-IC and JAXA are driven by topography, while
LPRM's are mainly controlled by vegetation. In addition, two
groups of opposite (positive/negative) effects from
topography and vegetation, topography and precipitation, and
precipitation and land surface temperature affect the
spatial variations of RUs in $CCI_A,$ RFSM, and ERA-Interim,
respectively. Meanwhile, more complex relationships are
found between multiple surface factors and RUs of different
products. In general, the underlying surface factors explain
on average $39.41\%$ and $28.34\%$ of the variations in RS
and LSM/LDAS SM RUs, respectively. Comparatively, the
near-ground meteorology factors have a slightly larger
effect on LSM/LDAS products than that on RS products.},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217)},
pid = {G:(DE-HGF)POF4-2173},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000619233200001},
doi = {10.1016/j.rse.2020.112225},
url = {https://juser.fz-juelich.de/record/904464},
}