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@ARTICLE{Shrestha:171936,
author = {Shrestha, P. and Sulis, M. and Masbou, M. and Kollet, S.
and Simmer, C.},
title = {{A} {S}cale-{C}onsistent {T}errestrial {S}ystems {M}odeling
{P}latform {B}ased on {COSMO}, {CLM}, and {P}ar{F}low},
journal = {Monthly weather review},
volume = {142},
number = {9},
issn = {1520-0493},
address = {Washington, DC [u.a.]},
publisher = {AMS87486},
reportid = {FZJ-2014-05490},
pages = {3466 - 3483},
year = {2014},
abstract = {A highly modular and scale-consistent Terrestrial Systems
Modeling Platform (TerrSysMP) is presented. The modeling
platform consists of an atmospheric model (Consortium for
Small-Scale Modeling; COSMO), a land surface model (the NCAR
Community Land Model, version 3.5; CLM3.5), and a 3D
variably saturated groundwater flow model (ParFlow). An
external coupler (Ocean Atmosphere Sea Ice Soil, version
3.0; OASIS3) with multiple executable approaches is employed
to couple the three independently developed component
models, which intrinsically allows for a separation of
temporal–spatial modeling scales and the coupling
frequencies between the component models.Idealized TerrSysMP
simulations are presented, which focus on the interaction of
key hydrologic processes, like runoff production (excess
rainfall and saturation) at different hydrological modeling
scales and the drawdown of the water table through
groundwater pumping, with processes in the atmospheric
boundary layer. The results show a strong linkage between
integrated surface–groundwater dynamics, biogeophysical
processes, and boundary layer evolution. The use of the
mosaic approach for the hydrological component model (to
resolve subgrid-scale topography) impacts simulated runoff
production, soil moisture redistribution, and boundary layer
evolution, which demonstrates the importance of hydrological
modeling scales and thus the advantages of the coupling
approach used in this study.Real data simulations were
carried out with TerrSysMP over the Rur catchment in
Germany. The inclusion of the integrated
surface–groundwater flow model results in systematic
patterns in the root zone soil moisture, which influence
exchange flux distributions and the ensuing atmospheric
boundary layer development. In a first comparison to
observations, the 3D model compared to the 1D model shows
slightly improved predictions of surface fluxes and a strong
sensitivity to the initial soil moisture content.},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {246 - Modelling and Monitoring Terrestrial Systems: Methods
and Technologies (POF2-246) / 255 - Terrestrial Systems:
From Observation to Prediction (POF3-255)},
pid = {G:(DE-HGF)POF2-246 / G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000341171100024},
doi = {10.1175/MWR-D-14-00029.1},
url = {https://juser.fz-juelich.de/record/171936},
}