Menno Straatsma

Dr. Menno Straatsma

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Research Focus & Metrics

Academic Career Length

21Years (2006-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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20 June 2018 in Geoscientific Model Development
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Journal Article
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ESEdwin Sutanudjaja
Edwin Sutanudjaja
RBRens van Beek
Rens van Beek
NWNiko Wanders
Niko Wanders
YWYoshihide Wada
Yoshihide Wada
JBJoyce H. C. Bosmans
Joyce H. C. Bosmans
MBMarc Bierkens
Marc Bierkens
We present PCR-GLOBWB 2, a global hydrology and water resources model. Compared to previous versions of PCR-GLOBWB, this version fully integrates water use. Sector-specific water demand, groundwater and surface water withdrawal, water consumption, and return flows are dynamically calculated at every time step and interact directly with the simulated hydrology. PCR-GLOBWB 2 has been fully rewritten in Python and PCRaster Python and has a modular structure, allowing easier replacement, maintenance, and development of model components. PCR-GLOBWB 2 has been implemented at 5 arcmin resolution, but a version parameterized at 30 arcmin resolution is also available. Both versions are available as open-source codes on https://github.com/UU-Hydro/PCR-GLOBWB_model (Sutanudjaja et al., 2017a). PCR-GLOBWB 2 has its own routines for groundwater dynamics and surface water routing. These relatively simple routines can alternatively be replaced by dynamically coupling PCR-GLOBWB 2 to a global two-layer groundwater model and 1-D–2-D hydrodynamic models. Here, we describe the main components of the model, compare results of the 30 and 5 arcmin versions, and evaluate their model performance using Global Runoff Data Centre discharge data. Results show that model performance of the 5 arcmin version is notably better than that of the 30 arcmin version. Furthermore, we compare simulated time series of total water storage (TWS) of the 5 arcmin model with those observed with GRACE, showing similar negative trends in areas of prevalent groundwater depletion. Also, we find that simulated total water withdrawal matches reasonably well with reported water withdrawal from AQUASTAT, while water withdrawal by source and sector provide mixed results.

1 March 2008 in Remote Sensing of Environment
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Journal Article
Closed access
MSMenno Straatsma
Menno Straatsma
MBM.J. Baptist
M.J. Baptist

1 March 2011 in Geomorphology
Verified
Journal Article
Closed access
KRK.A. Razak
K.A. Razak
MSMenno Straatsma
Menno Straatsma
CWC.J. van Westen
C.J. van Westen
Jean-Philippe MaletJean-Philippe Malet
Jean-Philippe Malet
SJSteven Michael De Jong
Steven Michael De Jong

1 July 2018 in ISPRS Journal of Photogrammetry and Remote Sensing
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Journal Article
Open access
WIWimala van Iersel
Wimala van Iersel
MSMenno Straatsma
Menno Straatsma
EAElisabeth Addink
Elisabeth Addink
HMHans Middelkoop
Hans Middelkoop

1 May 2013 in Geomorphology
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Journal Article
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KRKhamarrul Azahari Razak
Khamarrul Azahari Razak
MSMichele Santangelo
Michele Santangelo
CWCees J. Van Westen
Cees J. Van Westen
MSMenno Straatsma
Menno Straatsma
SJSteven Michael De Jong
Steven Michael De Jong

28 January 2020 in Environmental Research Letters
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Journal Article
Open access
LWLisa Watson
Lisa Watson
MSMenno Straatsma
Menno Straatsma
NWNiko Wanders
Niko Wanders
JVJudith A. Verstegen
Judith A. Verstegen
SJSteven Michael De Jong
Steven Michael De Jong
Derek KarssenbergDerek Karssenberg
Derek Karssenberg
Ecosystem service assessments facilitate the valuation of nature and support decision-making. Ecosystem services are connected to climate; however, ecosystem service values affected by climate change remain unclear. We mapped global ecosystem service values totaling ∼1.3 trillion international dollars for 2005. Transitions in Köppen–Geiger climate classes projected with General Circulation Models under the four IPCC Representative Concentration Pathways (RCP) were modeled providing 20 climate scenarios. The mapped global ecosystem service values were combined with the 20 climate scenarios in order to identify where and how much of the global ecosystem service value is within a climate class transition. By 2050, 252–375 billion international dollars of ecosystem service value (20%–30% of total value) are in a Köppen–Geiger climate transition for both RCP 2.6 and 8.5 scenarios. In RCP 2.6, the 2015 Paris Agreement carbon emission scenario target, Köppen–Geiger climate transitions stabilize after 2050. However, in the RCP 8.5 scenario, ecosystem service values amounting to 467–632 billion international dollars (37%–50% of total value) are in a Köppen–Geiger climate transition by 2085. These results provide an inclusive global overview of climate change impact on evaluated ecosystem services that affect populations and economies.