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@ARTICLE{Meyer:865571,
author = {Meyer, Thomas and Jagdhuber, Thomas and Piles, María and
Fink, Anita and Grant, Jennifer and Vereecken, Harry and
Jonard, François},
title = {{E}stimating gravimetric water content of a winter wheat
field from {L}-band vegetation optical depth},
journal = {Remote sensing},
volume = {11},
number = {20},
issn = {2072-4292},
address = {Basel},
publisher = {MDPI},
reportid = {FZJ-2019-04936},
pages = {2353 -},
year = {2019},
abstract = {A considerable amount of water is stored in vegetation,
especially in regions with high precipitation rates.
Knowledge of the vegetation water status is essential to
monitor changes in ecosystem health and to assess the
vegetation influence on the water budget. In this study, we
develop and validate an approach to estimate the gravimetric
vegetation water content (mg), defined as the amount of
water [kg] per wet biomass [kg], based on the attenuation of
microwave radiation through vegetation. mg is expected to be
more closely related to the actual water status of a plant
than the area-based vegetation water content (VWC), which
expresses the amount of water [kg] per unit area [m2]. We
conducted the study at the field scale over an entire growth
cycle of a winter wheat field. Tower-based L-band microwave
measurements together with in situ measurements of
vegetation properties (i.e., vegetation height, and mg for
validation) were performed. The results indicated a strong
agreement between the in situ measured and retrieved mg (R2
of 0.89), with mean and standard deviation (STD) values of
0.55 and 0.26 for the in situ measured mg and 0.57 and 0.19
for the retrieved mg, respectively. Phenological changes in
crop water content were captured, with the highest values of
mg obtained during the growth phase of the vegetation (i.e.,
when the water content of the plants and the biomass were
increasing) and the lowest values when the vegetation turned
fully senescent (i.e., when the water content of the plant
was the lowest). Comparing in situ measured mg and VWC, we
found their highest agreement with an R2 of 0.95 after
flowering (i.e., when the vegetation started to lose water)
and their main differences with an R2 of 0.21 during the
vegetative growth of the wheat vegetation (i.e., where the
mg was constant and VWC increased due to structural changes
in vegetation). In addition, we performed a sensitivity
analysis on the vegetation volume fraction (δ), an input
parameter to the proposed approach which represents the
volume percentage of solid plant material in air. This
δ-parameter is shown to have a distinct impact on the
thermal emission at L-band, but keeping δ constant during
the growth cycle of the winter wheat appeared to be valid
for these mg retrievals.},
cin = {IBG-3},
ddc = {620},
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:000498395800021},
doi = {10.3390/rs11202353},
url = {https://juser.fz-juelich.de/record/865571},
}