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@ARTICLE{Schwinger:17060,
author = {Schwinger, J. and Kollet, S. and Hoppe, C. and Elbern, H.},
title = {{S}ensitivity of {L}atent {H}eat fluxes to {I}nitial
{V}alues and {P}arameters of a {L}and-{S}urface {M}odel},
journal = {Vadose zone journal},
volume = {9},
issn = {1539-1663},
address = {Madison, Wis.},
publisher = {SSSA},
reportid = {PreJuSER-17060},
pages = {984 - 1001},
year = {2010},
note = {This work was funded by Deutsche Forschungsgemeinschaft
(DFG) in the framework of the SFB/TR 32 "Patterns in
Soil-Vegetation-Atmosphere Systems: Monitoring, Modeling and
Data Assimilation." The National Center for Atmospheric
Research (NCAR) is gratefully acknowledged for providing the
CLM source code and input data sets. The tangent linear CLM
source code was generated using the TAPENADE soft ware
provided by the Institut National de Recherche en
Informatique et en Automatique (INRIA). The authors thank
two anonymous reviewers for their constructive comments and
suggestions, which helped improve the manuscript.},
abstract = {A tangent linear version of the complex
soil-vegetation-atmosphere transfer model Community Land
Model has been developed and its ability to reproduce
relevant sensitivities of the modeled soil moisture and
latent heat flux (LE) evolution to a number of different
parameters on a short time scale (3 d) was analyzed. To this
end, a series of idealized experiments for different soil
moisture states and three different soil types was
conducted. We found that the tangent linear model performs
well for a large range of conditions. Situations in which
the linear approximation potentially fails were connected
with the occurrence of saturation and with the highly
nonlinear parameterization of water availability to plants.
The sensitivity of LE with respect to the model's initial
soil moisture state was calculated and compared with the LE
sensitivity to soil texture, leaf area index (LAI), and
vegetation roughness length. These sensitivities were found
to be highly variable with soil type and soil moisture. Our
results confirm that soil texture and LAI are key parameters
that have a dominant influence on modeled LE under specific
environmental conditions. As a preparatory study to soil
data assimilation developments, the results also serve to
quantify model uncertainties due to limited knowledge of
forcing processes and model parameters.},
keywords = {J (WoSType)},
cin = {IEK-8},
ddc = {550},
cid = {I:(DE-Juel1)IEK-8-20101013},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK491},
shelfmark = {Environmental Sciences / Soil Science / Water Resources},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000287739800016},
doi = {10.2136/vzj2009.0190},
url = {https://juser.fz-juelich.de/record/17060},
}