Boud Verbeiren

Prof. Dr. Boud Verbeiren

orcid

Research Focus & Metrics

Academic Career Length

23Years (2004-Present)

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

Representative Publications

View All Publications
2 February 2016 in Nature Geoscience
Verified
Journal Article
Closed access
ALAnne Van Loon
Anne Van Loon
TGTom Gleeson
Tom Gleeson
JCJulian Clark
Julian Clark
ADAlbert I. J. M. Van Dijk
Albert I. J. M. Van Dijk
KSKerstin Stahl
Kerstin Stahl
HLHenny A. J. Van Lanen
Henny A. J. Van Lanen

8 September 2016 in Hydrology and Earth System Sciences
Verified
Journal Article
Open access
PDF file
ALAnne Van Loon
Anne Van Loon
KSKerstin Stahl
Kerstin Stahl
GBGiuliano Di Baldassarre
Giuliano Di Baldassarre
JCJulian Clark
Julian Clark
SRSally Rangecroft
Sally Rangecroft
HLHenny A. J. Van Lanen
Henny A. J. Van Lanen
In the current human-modified world, or Anthropocene, the state of water stores and fluxes has become dependent on human as well as natural processes. Water deficits (or droughts) are the result of a complex interaction between meteorological anomalies, land surface processes, and human inflows, outflows, and storage changes. Our current inability to adequately analyse and manage drought in many places points to gaps in our understanding and to inadequate data and tools. The Anthropocene requires a new framework for drought definitions and research. Drought definitions need to be revisited to explicitly include human processes driving and modifying soil moisture drought and hydrological drought development. We give recommendations for robust drought definitions to clarify timescales of drought and prevent confusion with related terms such as water scarcity and overexploitation. Additionally, our understanding and analysis of drought need to move from single driver to multiple drivers and from uni-directional to multi-directional. We identify research gaps and propose analysis approaches on (1) drivers, (2) modifiers, (3) impacts, (4) feedbacks, and (5) changing the baseline of drought in the Anthropocene. The most pressing research questions are related to the attribution of drought to its causes, to linking drought impacts to drought characteristics, and to societal adaptation and responses to drought. Example questions include (i) What are the dominant drivers of drought in different parts of the world? (ii) How do human modifications of drought enhance or alleviate drought severity? (iii) How do impacts of drought depend on the physical characteristics of drought vs. the vulnerability of people or the environment? (iv) To what extent are physical and human drought processes coupled, and can feedback loops be identified and altered to lessen or mitigate drought? (v) How should we adapt our drought analysis to accommodate changes in the normal situation (i.e. what are considered normal or reference conditions) over time? Answering these questions requires exploration of qualitative and quantitative data as well as mixed modelling approaches. The challenges related to drought research and management in the Anthropocene are not unique to drought, but do require urgent attention. We give recommendations drawn from the fields of flood research, ecology, water management, and water resources studies. The framework presented here provides a holistic view on drought in the Anthropocene, which will help improve management strategies for mitigating the severity and reducing the impacts of droughts in future.

1 September 2015 in Journal of Hydrology: Regional Studies
Verified
Journal Article
Open access
ZZZ. Zomlot
Z. Zomlot
BVBoud Verbeiren
Boud Verbeiren
MHMarijke Huysmans
Marijke Huysmans
OBO. Batelaan
O. Batelaan
Study focusGroundwater is of strategic importance. The accurate estimation of groundwater recharge and assessing the fundamental controlling factors are therefore of utmost importance to protect groundwater systems. We used the spatially-distributed water-balance model WetSpass to estimate long-term average recharge in Flanders. We validated recharge rates with base flow estimates of 67 daily stream flow records using the hydrograph analyses. To this end we performed principal component analysis, multiple linear regression analysis and relative importance analysis to assess the controlling factors of the spatial variation of recharge and base flow with the influencing watershed characteristics.New hydrological insights for the regionThe average resulting recharge is 235mm/year and occurs mainly in winter. The overall moderate correlation between base flow estimates and modeled recharge rates indicates that base flow is a reasonable proxy of recharge. Groundwater recharge variation was explained in order of importance by precipitation, soil texture and vegetation cover; while base flow variation was strongly controlled by vegetation cover and groundwater depth. The results of this study highlight the important role of spatial variables in estimation of recharge and base flow. In addition, the prominent role of vegetation makes clear the potential importance of land-use changes on recharge and hence the need to include a proper strategy for land-use change in sustainable management of groundwater resources

28 November 2013 in Water Resources Management
Verified
Journal Article
Closed access
PDF file
GTGeorge Tsakiris
George Tsakiris
INI. Nalbantis
I. Nalbantis
HVH. Vangelis
H. Vangelis
BVBoud Verbeiren
Boud Verbeiren
MHMarijke Huysmans
Marijke Huysmans
OBOkke Batelaan
Okke Batelaan

1 October 2012 in International Journal of Applied Earth Observation and Geoinformation
Verified
Journal Article
Closed access
WEWiesam Essa
Wiesam Essa
BVBoud Verbeiren
Boud Verbeiren
Johannes van der KwastJohannes van der Kwast
Johannes van der Kwast
TVTim Van de Voorde
Tim Van de Voorde
OBOkke Batelaan
Okke Batelaan

27 February 2017 in Environmental Earth Sciences
Verified
Journal Article
Closed access
PDF file
KAKhodayar Abdollahi
Khodayar Abdollahi
IBImtiaz Bashir
Imtiaz Bashir
BVBoud Verbeiren
Boud Verbeiren
MHMahamane R. Harouna
Mahamane R. Harouna
AGAnn Van Griensven
Ann Van Griensven
OBOkke Batelaan
Okke Batelaan