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@INPROCEEDINGS{Naz:905604,
author = {Naz, Bibi and Sharples, Wendy and Kollet, Stefan and
Görgen, Klaus},
title = {{A} sensitivity analysis of hydrological states and fluxes
to groundwater representation in pan-{E}uropean multimodel
simulations.},
reportid = {FZJ-2022-00836},
year = {2021},
abstract = {High-resolution large-scale predictions of hydrologic
states and fluxes are important for many regional-scale
applications and water resource management. However, because
of uncertainties related to forcing data, model structural
errors arising from simplified representations of
hydrological processes or uncertain model parameters, model
simulations remain uncertain. To quantify this uncertainty,
multi-model simulations were performed at 3km resolution
over the European continent using the Community Land Model
(CLM3.5) and the ParFlow hydrologic model. The ParFlow model
simulates three-dimensional variably saturated groundwater
flow solving Richards equation and overland flow with a
two-dimensional kinematic wave approximation, whereas CLM3.5
applies a simple approach to simulate groundwater recharge
and discharge processes via the connection of bottom soil
layer and an unconfined aquifer. Over Europe with a lateral
resolution of 3km, both models were driven with the
COSMO-REA6 reanalysis dataset for the time period from 1997
to 2006 at an hourly time step using the same datasets for
the static input variables (such as topography, vegetation
and soil properties). Evaluation against independent
observations including satellite-derived and in-situ soil
moisture, evapotranspiration, and water table depth datasets
show that both models capture the interannual and seasonal
variations well at the regional scale, however ParFlow with
dynamic groundwater representation performs better in
simulating surface soil moisture in comparison with in-situ
data. Simulations with ParFlow have overall wetter soil
moisture than CLM, particularly in humid and cold regions
and driest soil moisture in the arid and semi-arid regions.
Moreover, the difference in ET between the two models shows
that ParFlow produced overall higher ET over the regions
with shallow water table and drier regions. This study helps
to understand and quantify uncertainties in groundwater
related processes in hydrologic simulations and resulting
implications for water resources assessment at regional to
continental scales.},
month = {Jun},
date = {2021-06-29},
organization = {ECMWF Global hydrological modelling
and forecasting, Online (UK), 29 Jun
2021 - 1 Jul 2021},
subtyp = {After Call},
cin = {IBG-3},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217) / EoCoE-II - Energy Oriented Center of Excellence
: toward exascale for energy (824158)},
pid = {G:(DE-HGF)POF4-2173 / G:(EU-Grant)824158},
typ = {PUB:(DE-HGF)24},
url = {https://juser.fz-juelich.de/record/905604},
}