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@ARTICLE{Naz:859669,
author = {Naz, Bibi S. and Kurtz, Wolfgang and Montzka, Carsten and
Sharples, Wendy and Görgen, Klaus and Keune, Jessica and
Gao, Huilin and Springer, Anne and Hendricks-Franssen,
Harrie-Jan and Kollet, Stefan},
title = {{I}mproving soil moisture and runoff simulations at 3 km
over {E}urope using land surface data assimilation},
journal = {Hydrology and earth system sciences},
volume = {23},
number = {1},
issn = {1607-7938},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2019-00511},
pages = {277 - 301},
year = {2019},
abstract = {Accurate and reliable hydrologic simulations are important
for many applications such as water resources management,
future water availability projections and predictions of
extreme events. However, the accuracy of water balance
estimates is limited by the lack of large-scale
observations, model simulation uncertainties and biases
related to errors in model structure and uncertain inputs
(e.g., hydrologic parameters and atmospheric forcings). The
availability of long-term and global remotely sensed soil
moisture offers the opportunity to improve model estimates
through data assimilation with complete spatiotemporal
coverage. In this study, we assimilated the European Space
Agency (ESA) Climate Change Initiative (CCI) derived soil
moisture (SM) information to improve the estimation of
continental-scale soil moisture and runoff. The assimilation
experiment was conducted over a time period 2000–2006 with
the Community Land Model, version 3.5 (CLM3.5), integrated
with the Parallel Data Assimilation Framework (PDAF) at a
spatial resolution of 0.0275∘ (∼3 km) over Europe. The
model was forced with the high-resolution reanalysis
COSMO-REA6 from the Hans Ertel Centre for Weather Research
(HErZ). The performance of assimilation was assessed against
open-loop model simulations and cross-validated with
independent ESA CCI-derived soil moisture (CCI-SM) and
gridded runoff observations. Our results showed improved
estimates of soil moisture, particularly in the summer and
autumn seasons when cross-validated with independent CCI-SM
observations. The assimilation experiment results also
showed overall improvements in runoff, although some regions
were degraded, especially in central Europe. The results
demonstrated the potential of assimilating satellite soil
moisture observations to produce downscaled and improved
high-resolution soil moisture and runoff simulations at the
continental scale, which is useful for water resources
assessment and monitoring.},
cin = {IBG-3 / JARA-HPC / JSC},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118 / $I:(DE-82)080012_20140620$ /
I:(DE-Juel1)JSC-20090406},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255) / EoCoE - Energy oriented Centre of Excellence
for computer applications (676629) / IRTG, Graduate School -
Patterns in Soil-Vegetation-Atmosphere-Systems: Monitoring,
Modelling and Data Assimilation (TR32) (IRTG, Graduate
School) (IRTG-GRADUATE-20170406) / Water4Enery
$(jibg31_20160501)$ / 511 - Computational Science and
Mathematical Methods (POF3-511)},
pid = {G:(DE-HGF)POF3-255 / G:(EU-Grant)676629 /
G:(DE-Juel1)IRTG-GRADUATE-20170406 /
$G:(DE-Juel1)jibg31_20160501$ / G:(DE-HGF)POF3-511},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000456148000001},
doi = {10.5194/hess-23-277-2019},
url = {https://juser.fz-juelich.de/record/859669},
}