% 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{Idrissou:878071,
author = {Idrissou, Mouhamed and Diekkrüger, Bernd and Tischbein,
Bernhard and Ibrahim, Boubacar and Yira, Yacouba and Steup,
Gero and Poméon, Thomas},
title = {{T}esting the {R}obustness of a {P}hysically-{B}ased
{H}ydrological {M}odel in {T}wo {D}ata {L}imited {I}nland
{V}alley {C}atchments in {D}ano, {B}urkina {F}aso},
journal = {Hydrology},
volume = {7},
number = {3},
issn = {2306-5338},
address = {Basel},
publisher = {MDPI},
reportid = {FZJ-2020-02613},
pages = {43 -},
year = {2020},
abstract = {This study investigates the robustness of the
physically-based hydrological model WaSiM (water balance and
flow simulation model) for simulating hydrological processes
in two data sparse small-scale inland valley catchments
(Bankandi-Loffing and Mebar) in Burkina Faso. An intensive
instrumentation with two weather stations, three rain
recorders, 43 piezometers, and one soil moisture station was
part of the general effort to reduce the scarcity of
hydrological data in West Africa. The data allowed us to
successfully parameterize, calibrate (2014–2015), and
validate (2016) WaSiM for the Bankandi-Loffing catchment.
Good model performance concerning discharge in the
calibration period (R2 = 0.91, NSE = 0.88, and KGE = 0.82)
and validation period (R2 = 0.82, NSE = 0.77, and KGE =
0.57) was obtained. The soil moisture (R2 = 0.7, NSE = 0.7,
and KGE = 0.8) and the groundwater table (R2 = 0.3, NSE =
0.2, and KGE = 0.5) were well simulated, although not
explicitly calibrated. The spatial transposability of the
model parameters from the Bankandi-Loffing model was
investigated by applying the best parameter-set to the Mebar
catchment without any recalibration. This resulted in good
model performance in 2014–2015 (R2 = 0.93, NSE = 0.92, and
KGE = 0.84) and in 2016 (R2 = 0.65, NSE = 0.64, and KGE =
0.59). This suggests that the parameter-set achieved in this
study can be useful for modeling ungauged inland valley
catchments in the region. The water balance shows that
evaporation is more important than transpiration $(76\%$ and
$24\%,$ respectively, of evapotranspiration losses) and the
surface flow is very sensitive to the observed high
interannual variability of rainfall. Interflow dominates the
uplands, but base flow is the major component of stream flow
in inland valleys. This study provides useful information
for the better management of soil and scarce water resources
for smallholder farming in the area},
cin = {IBG-3},
ddc = {550},
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)16},
UT = {WOS:000580133600001},
doi = {10.3390/hydrology7030043},
url = {https://juser.fz-juelich.de/record/878071},
}