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@ARTICLE{Huang:875091,
author = {Huang, Yafei and Hendricks-Franssen, Harrie-Jan and Herbst,
Michael and Hirschi, Martin and Michel, Dominik and
Seneviratne, Sonia I. and Teuling, Adriaan J. and Vogt,
Roland and Detlef, Schumacher and Pütz, Thomas and
Vereecken, Harry},
title = {{E}valuation of different methods for gap filling of
long‐term actual evapotranspiration time series measured
by lysimeters},
journal = {Vadose zone journal},
volume = {19},
number = {1},
issn = {1539-1663},
address = {Alexandria, Va.},
publisher = {GeoScienceWorld},
reportid = {FZJ-2020-01798},
pages = {1-15},
year = {2020},
abstract = {Terrestrial evapotranspiration (ET) is the second largest
water flux in the global water cycle. It can be measured
with different techniques; weighable lysimeters can provide
very accurate measurements, and some very long‐term time
series exist. However, these lysimeter time series are
affected by data gaps that must be filled to estimate actual
ET totals and long‐term trends. In this paper, we explore
four different gap‐filling methods: the potential
ET‐method, the ratio method, the FAO‐based water balance
method, and HYDRUS modeling. These gap‐filling methods
were evaluated for three time series of actual ET measured
by lysimeters and meteorological data of three European
sites. Separate evaluations were made for the five driest
and five wettest April–October periods to investigate
whether the performance of the gap‐filling methods was
affected by hydrological conditions. Series of random gaps
were artificially created for the three time series,
including gaps of four different lengths. Actual ET was
estimated for these gaps with the gap‐filling methods,
which were evaluated based on RMSE and mean bias error. The
results show that the ratio method outperformed other
methods for gap filling of lysimeter data for Basel
(Switzerland), whereas the HYDRUS method outperformed other
methods for Rheindahlen (Germany). For Rietholzbach
(Switzerland), the different methods performed very
similarly, except that the FAO method gives slightly larger
RMSEs. The gap‐filling methods do not perform very
differently for dry and wet conditions. The ratio method is
recommended for filling smaller gaps, and the HYDRUS method
is recommended for longer gaps of 30 d.},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000618773300020},
doi = {10.1002/vzj2.20020},
url = {https://juser.fz-juelich.de/record/875091},
}