% 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”.
@ARTICLE{Wiekenkamp:820924,
author = {Wiekenkamp, I. and Huisman, J. A. and Bogena, Heye and
Graf, Alexander and Lin, H. S. and Drüe, C. and Vereecken,
H.},
title = {{C}hanges in measured spatiotemporal patterns of
hydrological response after partial deforestation in a
headwater catchment},
journal = {Journal of hydrology},
volume = {542},
issn = {0022-1694},
address = {Amsterdam [u.a.]},
publisher = {Elsevier},
reportid = {FZJ-2016-06188},
pages = {648 - 661},
year = {2016},
abstract = {Although the hydrological effects of land use change have
been studied extensively, only few datasets are available to
accurately describe, model, and predict detailed changes in
spatiotemporal patterns of hydrological fluxes and states
due to land use change. The Wüstebach catchment within the
TERENO (TERrestrial Environmental Observatories) network in
Germany provides a unique monitoring setup to measure the
major components of the water balance (evapotranspiration,
discharge, precipitation) and the spatiotemporal
distribution of soil moisture before and after a partial
deforestation. Here, we present five years of measured
hydrological data, including all major water budget
components three years before and two years after a partial
deforestation. A data-driven approach was used to understand
changes and related feedback mechanisms in spatiotemporal
hydrological response patterns. As expected from earlier
studies, the partial deforestation caused a decrease in
evapotranspiration and an increase in discharge. A closer
look at the high resolution datasets revealed new insights
in the intra-annual variability and relationship between the
water balance components. The overall decrease in
evapotranspiration caused a large increase in soil water
storage in the deforested region, especially during the
summer period, which in turn caused an increase in the
frequency of high discharge in the same period. Although the
evapotranspiration in the forested region was larger on
average, the deforested region showed a higher
evapotranspiration during part of the summer period. This
could be related to wetter conditions in the deforested
area, accompanied with the emergence of grass vegetation. At
the same time, wetter soil moisture conditions in the
deforested area increased the spatial variance of soil
moisture in the summer and therewith altered the
relationship between spatial mean and variance. Altogether,
this study illustrates that detailed spatiotemporal
monitoring can provide new insights into the hydrological
effects of partial deforestation.},
cin = {IBG-3},
ddc = {690},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255) / DFG project 15232683 - TRR 32: Muster und
Strukturen in Boden-Pflanzen-Atmosphären-Systemen:
Erfassung, Modellierung und Datenassimilation (15232683) /
IDAS-GHG - Instrumental and Data-driven Approaches to
Source-Partitioning of Greenhouse Gas Fluxes: Comparison,
Combination, Advancement (BMBF-01LN1313A)},
pid = {G:(DE-HGF)POF3-255 / G:(GEPRIS)15232683 /
G:(DE-Juel1)BMBF-01LN1313A},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000388248400047},
doi = {10.1016/j.jhydrol.2016.09.037},
url = {https://juser.fz-juelich.de/record/820924},
}