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@ARTICLE{Belleflamme:1007830,
author = {Belleflamme, Alexandre and Görgen, Klaus and Wagner,
Niklas and Kollet, Stefan and Bathiany, Sebastian and El
Zohbi, Juliane and Rechid, Diana and Vanderborght, Jan and
Vereecken, Harry},
title = {{H}ydrological forecasting at impact scale: the integrated
{P}ar{F}low hydrological model at 0.6 km for climate
resilient water resource management over {G}ermany},
journal = {Frontiers in water},
volume = {5},
issn = {2624-9375},
address = {Lausanne},
publisher = {Frontiers Media},
reportid = {FZJ-2023-02215},
pages = {1183642},
year = {2023},
abstract = {In the context of the repeated droughts that have affected
central Europe over the last years (2018–2020, 2022),
climate-resilient management of water resources, based on
timely information about the current state of the
terrestrial water cycle and forecasts of its evolution, has
gained an increasing importance. To achieve this, we propose
a new setup for simulations of the terrestrial water cycle
using the integrated hydrological model ParFlow/CLM at high
spatial and temporal resolution (i.e., 0.611 km, hourly time
step) over Germany and the neighboring regions. We show that
this setup can be used as a basis for a monitoring and
forecasting system that aims to provide stakeholders from
many sectors, but especially agriculture, with diagnostics
and indicators highlighting different aspects of subsurface
water states and fluxes, such as subsurface water storage,
seepage water, capillary rise, or fraction of plant
available water for different (root-)depths. The validation
of the new simulation setup with observation-based data
monthly over the period 2011–2020 yields good results for
all major components of the terrestrial water cycle analyzed
here, i.e., volumetric soil moisture, evapotranspiration,
water table depth, and river discharge. As this setup relies
on a standardized grid definition and recent globally
available static fields and parameters (e.g., topography,
soil hydraulic properties, land cover), the workflow could
easily be transferred to many regions of the Earth,
including sparsely gauged regions, since ParFlow/CLM does
not require calibration.},
cin = {IBG-3},
ddc = {333.7},
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:001007969000001},
doi = {10.3389/frwa.2023.1183642},
url = {https://juser.fz-juelich.de/record/1007830},
}