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@PHDTHESIS{Ali:843656,
author = {Ali, Muhammad},
title = {{S}patio-{T}emporal {E}stimation and {V}alidation of
{R}emotely {S}ensed {V}egetation and {H}ydrological {F}luxes
in the {R}ur {C}atchment, {G}ermany},
volume = {403},
school = {Universität Bonn},
type = {Dissertation},
address = {Jülich},
publisher = {Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag},
reportid = {FZJ-2018-01225},
isbn = {978-3-95806-287-0},
series = {Schriften des Forschungszentrums Jülich Reihe Energie $\&$
Umwelt / Energy $\&$ Environment},
pages = {116 S.},
year = {2018},
note = {Universität Bonn, Diss., 2017},
abstract = {Operational availability of spatio-temporal vegetation and
hydrological estimates are becoming increasingly attractive
for hydrologic studies from local through regional and
global scales, especially in remote areas and ungauged
basins. More advancement and versatility in satellite-based
remotely sensed methods towards consistent and timely
information for monitoring regional scale vegetation and
hydrological fluxes may lead to efficient and unprecedented
planning and management of agricultural practices and water
resources. This thesis develops and analyses remote sensing
methods for regional scale vegetation and land surface water
fluxes estimation. Results from this study are validated at
various test sites in the Rur catchment, Germany. These
sites are equipped with sophisticated and state-of-the-art
instruments for monitoring vegetation and hydrological
fluxes. Second chapter in this thesis explains a direct
retrieval method and validation of the Leaf Area Index (LAI)
from time-series of multispectral RapidEye images. LAI,
quantifying the amount of leaf material, considered as an
important variable for numerous processes in hydrological
studies that link vegetation to climate. $\textit{In situ}$
LAI measuring methods have the limitation of being labor
intensive and site specific. Remote sensing LAI
(LAI$_{rapideye}$) were derived using different vegetation
indices, namely SAVI (Soil Adjusted Vegetation Index) and
NDVI (Normalized Difference Vegetation Index). Additionally,
applicability of the newly available red-edge band (RE) was
also analyzed through Normalized Difference Red-Edge index
(NDRE) and Soil Adjusted Red-Edge index (SARE). The
LAI$_{rapideye}$ obtained from vegetation indices with
red-edge band showed better correlation with destructive
LAI$_{destr}$ (r = 0.88 and Root Mean Square Deviation, RMSD
= 1.01 \& 0.92) than LAI from vegetation indices without
red-edge band. This study also investigated the need to
apply relative and absolute atmospheric correction methods
to the time-series of RapidEye Level 3A data prior to LAI
estimation. Analysis of the RapidEye data set showed that
application of the atmospheric corrections did not improve
correlation of the estimated LAI with in situ LAI, because
RapidEye Level 3A data are provided with simplified
atmospheric corrections and the vegetation indices used for
LAI retrieval ware already normalized. Third chapter
investigates estimation of spatio-temporal latent heat using
an energy balance approach and simplified regression between
calculated latent heat (from energy balance) and downward
shortwave radiation data from the Spinning Enhanced Visible
and Infrared Imager (SEVIRI) onboard Meteosat Second
Generation (MSG) Satellites. Mapping the spatio-temporal
[...]},
cin = {IBG-3},
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)3 / PUB:(DE-HGF)11},
urn = {urn:nbn:de:0001-2018030704},
url = {https://juser.fz-juelich.de/record/843656},
}