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@ARTICLE{Ma:902254,
author = {Ma, Yueling and Montzka, Carsten and Bayat, Bagher and
Kollet, Stefan},
title = {{A}n {I}ndirect {A}pproach {B}ased on {L}ong {S}hort-{T}erm
{M}emory {N}etworks to {E}stimate {G}roundwater {T}able
{D}epth {A}nomalies {A}cross {E}urope {W}ith an
{A}pplication for {D}rought {A}nalysis},
journal = {Frontiers in water},
volume = {3},
issn = {2624-9375},
address = {Lausanne},
publisher = {Frontiers Media},
reportid = {FZJ-2021-04124},
pages = {723548},
year = {2021},
abstract = {The lack of high-quality continental-scale groundwater
table depth observations necessitates developing an indirect
method to produce reliable estimation for water table depth
anomalies (wtda) over Europe to facilitate European
groundwater management under drought conditions. Long
Short-Term Memory (LSTM) networks are a deep learning
technology to exploit long-short-term dependencies in the
input-output relationship, which have been observed in the
response of groundwater dynamics to atmospheric and land
surface processes. Here, we introduced different input
variables including precipitation anomalies (pra), which is
the most common proxy of wtda, for the networks to arrive at
improved wtda estimates at individual pixels over Europe in
various experiments. All input and target data involved in
this study were obtained from the simulated TSMP-G2A data
set. We performed wavelet coherence analysis to gain a
comprehensive understanding of the contributions of
different input variable combinations to wtda estimates.
Based on the different experiments, we derived an indirect
method utilizing LSTM networks with pra and soil moisture
anomaly (θa) as input, which achieved the optimal network
performance. The regional medians of test R2 scores and
RMSEs obtained by the method in the areas with wtd ≤ 3.0 m
were $76\%-95\%$ and 0.17-0.30, respectively, constituting a
$20\%-66\%$ increase in median R2 and a 0.19-0.30 decrease
in median RMSEs compared to the LSTM networks only with pra
as input. Our results show that introducing θa
significantly improved the performance of the trained
networks to predict wtda, indicating the substantial
contribution of θa to explain groundwater anomalies. Also,
the European wtda map reproduced by the method had good
agreement with that derived from the TSMP-G2A data set with
respect to drought severity, successfully detecting $~41\%$
of strong drought events (wtda ≥ 1.5) and $~29\%$ of
extreme drought events (wtda ≥ 2) in August 2015. The
study emphasizes the importance to combine soil moisture
information with precipitation information in quantifying or
predicting groundwater anomalies. In the future, the
indirect method derived in this study can be transferred to
real-time monitoring of groundwater drought at the
continental scale using remotely sensed soil moisture and
precipitation observations or respective information from
weather prediction models.},
cin = {IBG-3},
ddc = {333.7},
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:000720866900001},
doi = {10.3389/frwa.2021.723548},
url = {https://juser.fz-juelich.de/record/902254},
}