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@ARTICLE{Hasan:153465,
author = {Hasan, Sayeh and Montzka, Carsten and Rüdiger, Christoph
and Ali, Muhammed and Bogena, Heye and Vereecken, Harry},
title = {{S}oil moisture retrieval from airborne {L}-band passive
microwave using high resolution multispectral data},
journal = {ISPRS journal of photogrammetry and remote sensing},
volume = {91},
issn = {0924-2716},
address = {Amsterdam [u.a.]},
publisher = {Elsevier},
reportid = {FZJ-2014-03063},
pages = {59 - 71},
year = {2014},
abstract = {For the soil moisture retrieval from passive microwave
sensors, such as ESA’s Soil Moisture and Ocean Salinity
(SMOS) and the NASA Soil Moisture Active and Passive (SMAP)
mission, a good knowledge about the vegetation
characteristics is indispensable. Vegetation cover is a
principal factor in the attenuation, scattering and
absorption of the microwave emissions from the soil; and has
a direct impact on the brightness temperature by way of its
canopy emissions. Here, brightness temperatures were
measured at three altitudes across the TERENO (Terrestrial
Environmental Observatories) Rur catchment site in Germany
to achieve a range of spatial resolutions using the airborne
Polarimetric L-band Multibeam Radiometer 2 (PLMR2). The
L-band Microwave Emission of the Biosphere (L-MEB) model
which simulates microwave emissions from the
soil–vegetation layer at L-band was used to retrieve
surface soil moisture for all resolutions. A Monte Carlo
approach was developed to simultaneously estimate soil
moisture and the vegetation parameter b’ describing the
relationship between the optical thickness τ and the Leaf
Area Index (LAI). LAI was retrieved from multispectral
RapidEye imagery and the plant specific vegetation parameter
b′ was estimated from the lowest flight altitude data for
crop, grass, coniferous forest, and deciduous forest. Mean
values of b’ were found to be 0.18, 0.07, 0.26 and 0.23,
respectively. By assigning the estimated b′ to higher
flight altitude data sets, a high accuracy soil moisture
retrieval was achieved with a Root Mean Square Difference
(RMSD) of 0.035 m3 m−3 when compared to ground-based
measurements.},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {246 - Modelling and Monitoring Terrestrial Systems: Methods
and Technologies (POF2-246) / 255 - Terrestrial Systems:
From Observation to Prediction (POF3-255)},
pid = {G:(DE-HGF)POF2-246 / G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000335104700005},
doi = {10.1016/j.isprsjprs.2014.02.005},
url = {https://juser.fz-juelich.de/record/153465},
}