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@ARTICLE{Scheiffele:889191,
author = {Scheiffele, Lena M. and Baroni, Gabriele and Franz, Trenton
E. and Jakobi, Jannis and Oswald, Sascha E.},
title = {{A} profile shape correction to reduce the vertical
sensitivity of cosmic‐ray neutron sensing of soil
moisture},
journal = {Vadose zone journal},
volume = {19},
number = {1},
issn = {1539-1663},
address = {Hoboken, NJ},
publisher = {Wiley},
reportid = {FZJ-2021-00101},
pages = {e20083},
year = {2020},
abstract = {In recent years, cosmic‐ray neutron sensing (CRNS) has
shown a large potential among proximal sensing techniques to
monitor soil moisture noninvasively, with high frequency and
a large support volume (radius up to 240 m and sensing depth
up to 80 cm). This signal is, however, more sensitive to
closer distances and shallower depths. Inherently,
CRNS‐derived soil moisture is a spatially weighted value,
different from an average soil moisture as retrieved by a
sensor network. In this study, we systematically test a new
profile shape correction on CRNS‐derived soil moisture,
based on additional soil moisture profile measurements and
vertical unweighting, which is especially relevant during
pronounced wetting or drying fronts. The analyses are
conducted with data collected at four contrasting field
sites, each equipped with a CRNS probe and a distributed
soil moisture sensor network. After applying the profile
shape correction on CRNS‐derived soil moisture, it is
compared with the sensor network average. Results show that
the influence of the vertical sensitivity of CRNS on
integral soil moisture values is successfully reduced. One
to three properly located profile measurements within the
CRNS support volume improve the performance. For the four
investigated field sites, the RMSE decreased $11–53\%$
when only one profile location was considered. We therefore
recommend to install along with a CRNS at least one soil
moisture profile in a radial distance <100 m and a
measurement depth down to 50 cm.
Profile‐shape‐corrected, CRNS‐derived soil moisture is
an unweighted integral soil moisture over the support
volume, which is easier to interpret and easier to use for
further applications.},
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:000618773300076},
doi = {10.1002/vzj2.20083},
url = {https://juser.fz-juelich.de/record/889191},
}