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@ARTICLE{Ma:893348,
author = {Ma, Yueling and Montzka, Carsten and Bayat, Bagher and
Kollet, Stefan},
title = {{U}sing {L}ong {S}hort-{T}erm {M}emory networks to connect
water table depth anomalies to precipitation anomalies over
{E}urope},
journal = {Hydrology and earth system sciences},
volume = {25},
number = {6},
issn = {1607-7938},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2021-02700},
pages = {3555 - 3575},
year = {2021},
abstract = {Many European countries rely on groundwater for public and
industrial water supply. Due to a scarcity of near-real-time
water table depth (wtd) observations, establishing a
spatially consistent groundwater monitoring system at the
continental scale is a challenge. Hence, it is necessary to
develop alternative methods for estimating wtd anomalies
(wtda) using other hydrometeorological observations
routinely available near real time. In this work, we explore
the potential of Long Short-Term Memory (LSTM) networks for
producing monthly wtda using monthly precipitation anomalies
(pra) as input. LSTM networks are a special category of
artificial neural networks that are useful for detecting a
long-term dependency within sequences, in our case time
series, which is expected in the relationship between pra
and wtda. In the proposed methodology, spatiotemporally
continuous data were obtained from daily terrestrial
simulations of the Terrestrial Systems Modeling Platform
(TSMP) over Europe (hereafter termed the TSMP-G2A data set),
with a spatial resolution of 0.11°, ranging from the years
1996 to 2016. The data were separated into a training set
(1996–2012), a validation set (2013–2014), and a test
set (2015–2016) to establish local networks at selected
pixels across Europe. The modeled wtda maps from LSTM
networks agreed well with TSMP-G2A wtda maps on spatially
distributed dry and wet events, with 2003 and 2015
constituting drought years over Europe. Moreover, we
categorized the test performances of the networks based on
intervals of yearly averaged wtd, evapotranspiration (ET),
soil moisture (θ), snow water equivalent (Sw), soil type
(St), and dominant plant functional type (PFT). Superior
test performance was found at the pixels with
wtd < 3 m, ET > 200 mm, θ>0.15 m3 m−3,
and Sw<10 mm, revealing a significant impact of the local
factors on the ability of the networks to process
information. Furthermore, results of the cross-wavelet
transform (XWT) showed a change in the temporal pattern
between TSMP-G2A pra and wtda at some selected pixels, which
can be a reason for undesired network behavior. Our results
demonstrate that LSTM networks are useful for producing
high-quality wtda based on other hydrometeorological data
measured and predicted at large scales, such as pra. This
contribution may facilitate the establishment of an
effective groundwater monitoring system over Europe that is
relevant to water management.},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217) / ERA-PLANET - The European network for observing
our changing planet (689443)},
pid = {G:(DE-HGF)POF4-2173 / G:(EU-Grant)689443},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000667601500002},
doi = {10.5194/hess-25-3555-2021},
url = {https://juser.fz-juelich.de/record/893348},
}