% IMPORTANT: The following is UTF-8 encoded. This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.
@PHDTHESIS{Steenpa:139798,
author = {Steenpaß, Christian},
title = {{C}oupled modeling of water, vapor and heat in unsaturated
soils – {F}ield applications and numerical studies},
volume = {167},
school = {RWTH Aachen},
type = {Dissertation},
address = {Jülich},
publisher = {Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag},
reportid = {FZJ-2013-05769},
isbn = {978-3-89336-854-9},
series = {Schriften des Forschungszentrums Jülich . Reihe Energie
$\&$ Umwelt / Energy $\&$ Environment},
pages = {X, 123 S.},
year = {2013},
note = {Dissertation, RWTH Aachen, 2013},
abstract = {The present work is part of the Sonderforschungsbereich
TransregioCollaborative Research Center 32 (SFB/TR32). This
interdisciplinary research projectfocuses on interaction of
energy, water, and carbon between the domains of
soil,vegetation, and lower atmosphere and resulting patterns
of state variables. Soilsurface water content and
temperature patterns provide the lower boundary
foratmospheric and the upper boundary for hydrologic
problems, making the soil surfacean important interface
between both domains. Because of the strong non-linearity
ofsoil hydraulic properties (SHP), measureable soil water
content and, directly linked byevaporation, temperature
patterns develop even at relatively small scales of a
fewdecimeters. This link between temperature and water
content and the resultingformation of measureable patterns
within soils makes consideration of coupled heatand water
fluxes inevitable when trying to simulate or predict
underlying processes.The present work was conducted in the
first research period of SFB TR 32 and focuswas on near
surface fluxes and patterns in bare soils. Within this
context, the presentthesis consists of three key
objectives:First, the influence of neglecting thermal
effects on instantaneous fluxes suchas diurnal evaporation
and on state variables such as surface temperature and
watercontent is studied. Over a period of five days,
evaporation, water content andtemperature were calculated
using a coupled and an uncoupled modeling approach.Measured
meteorological data were taken as upper boundary condition.
Both modelswere run assuming wet and dry initial conditions.
Results show that with wet initialconditions, differences
between coupled and uncoupled approach are negligible. In
adry soil, differences in actual evaporation rate in both
model approaches resulted inrelatively large differences in
modeled soil surface temperatures (SST). In the upperpart of
the soil, influence of thermal and isothermal vapor flux
components has asignificant effect on the total net water
flux (as entirety of liquid water and vapor).Furthermore,
the enhancement factor (Cass et al. 1984) used to
compensate},
keywords = {Dissertation (GND)},
cin = {IBG-3},
ddc = {500},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {246 - Modelling and Monitoring Terrestrial Systems: Methods
and Technologies (POF2-246) / DFG project 15232683 - TRR 32:
Muster und Strukturen in
Boden-Pflanzen-Atmosphären-Systemen: Erfassung,
Modellierung und Datenassimilation (15232683)},
pid = {G:(DE-HGF)POF2-246 / G:(GEPRIS)15232683},
typ = {PUB:(DE-HGF)3 / PUB:(DE-HGF)11},
url = {https://juser.fz-juelich.de/record/139798},
}