Laurène Bouaziz

ORCID: 0000-0003-0597-8051
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About
Contact & Profiles
Research Areas
  • Hydrology and Watershed Management Studies
  • Flood Risk Assessment and Management
  • Plant Water Relations and Carbon Dynamics
  • Soil erosion and sediment transport
  • Hydrology and Drought Analysis
  • Hydrological Forecasting Using AI
  • Soil Moisture and Remote Sensing
  • Hydrology and Sediment Transport Processes
  • Climate variability and models
  • Cryospheric studies and observations
  • Peatlands and Wetlands Ecology
  • Ionosphere and magnetosphere dynamics
  • Water resources management and optimization
  • Evaluation and Performance Assessment
  • Case Reports on Hematomas
  • Trauma and Emergency Care Studies
  • Landslides and related hazards
  • Meteorological Phenomena and Simulations
  • Groundwater flow and contamination studies
  • Earthquake Detection and Analysis
  • Transboundary Water Resource Management
  • Southeast Asian Sociopolitical Studies
  • Soil and Water Nutrient Dynamics
  • Asian Geopolitics and Ethnography
  • Environmental Monitoring and Data Management

Deltares
2015-2024

Delft University of Technology
2016-2022

Environmental and Water Resources Engineering
2021

Abstract. Intercatchment groundwater flows (IGFs), defined as across topographic divides, can occur regional that bypass headwater streams and only drain into the channel further downstream or directly to sea. However, also be diverted adjacent river basins due geological features (e.g., faults, dipping beds highly permeable conduits). Even though intercatchment a significant part of water balance, they are often not considered in hydrological studies. Yet, assuming this process negligible...

10.5194/hess-22-6415-2018 article EN cc-by Hydrology and earth system sciences 2018-12-10

Abstract. Streamflow is often the only variable used to evaluate hydrological models. In a previous international comparison study, eight research groups followed an identical protocol calibrate 12 models using observed streamflow of catchments within Meuse basin. current we quantify differences in five states and fluxes these process-based with similar performance, systematic comprehensive way. Next, assess model behavior plausibility by ranking for set criteria remote-sensing data...

10.5194/hess-25-1069-2021 article EN cc-by Hydrology and earth system sciences 2021-03-02

Abstract. Future hydrological behavior in a changing world is typically predicted based on models that are calibrated past observations, disregarding systems and, therefore, model parameters may change as well. In reality, experience almost continuous over wide spectrum of temporal and spatial scales. particular, there growing evidence vegetation adapts to climatic conditions by adjusting its root zone storage capacity, which the key parameter any terrestrial system. addition, other species...

10.5194/hess-26-1295-2022 article EN cc-by Hydrology and earth system sciences 2022-03-09

Many impact assessment studies rely on hydrological and hydrodynamic (hydro) models.These models typically require a large set of parameters derived from different datasets hence manual setup can be time consuming hard to reproduce.HydroMT (Hydro Model Tools) is an open-source Python package that aims make the process building model instances analyzing results automated reproducible.The provides common interface data instances, workflows transform into based (hydrological) GIS statistical...

10.21105/joss.04897 article EN cc-by The Journal of Open Source Software 2023-03-07

Abstract The spatiotemporal dynamics of water volumes stored in the unsaturated root zone are a key control on response terrestrial hydrological systems. Robust, catchment‐scale root‐zone soil moisture estimates thus critical for reliable predictions river flow, groundwater recharge, or evaporation. Satellites provide near‐surface that can be used to approximate content entire through Soil Water Index (SWI). characteristic time length ( T , days), as only parameter SWI approach,...

10.1029/2019wr026365 article EN cc-by Water Resources Research 2020-03-01

Abstract. The wflow_sbm hydrological model, recently released by Deltares, as part of the Wflow.jl (v0.7.3) modelling framework, is being used to better understand and potentially address multiple operational water resource planning challenges from a catchment scale national continental global scale. free open-source distributed framework written in Julia programming language. development wflow_sbm, model structure, equations functionalities are described detail, including example...

10.5194/gmd-17-3199-2024 article EN cc-by Geoscientific model development 2024-04-25

Abstract. International collaboration between research institutes and universities is a promising way to reach consensus on hydrological model development. Although comparison studies are very valuable for international cooperation, they do often not lead clear new insights regarding the relevance of modelled processes. We hypothesise that this partly caused by complexity methods used, which focus too much good overall performance instead focusing variety specific events. In study, we use an...

10.5194/hess-21-423-2017 article EN cc-by Hydrology and earth system sciences 2017-01-25

This study investigates the influence of DEM resolutions on flood inundation simulation. Sanyei drainage area Tainan City is taken as a case study. The catchment 43.7 km2 with main stream 6.7km and elevations running from 2 m to 30 m. uses 1x1 LiDAR basis. To do pure 2D simulation, channel elevation adjusted based cross-sectional measurements. 1x1m later used basis aggregate several DEMs including: 5x5m, 10x10m, 20x20m, 40x40m. Five models were built 5 mentioned above same model setting....

10.1016/j.proeng.2016.07.435 article EN Procedia Engineering 2016-01-01

Abstract. Streamflow is often the only variable used to constrain hydrological models. In a previous international comparison study, eight research groups followed an identical protocol calibrate total of twelve models using observed streamflow catchments within Meuse basin. current we hypothesize that these process-based with similar performance have representations internal states and fluxes. We test our hypothesis by comparing fluxes between assess their plausibility remotely-sensed...

10.5194/hess-2020-176 preprint EN cc-by 2020-04-28

Abstract. The wflow_sbm hydrologic model, recently released by Deltares, as part of the Wflow.jl (v0.6.1) modelling framework is being used to better understand and potentially address multiple operational water resources planning challenges from catchment scale, national scale continental global scale. a free open-source distributed written in Julia programming language. development wflow_sbm, model structure, equations functionalitities are described detail, including example applications...

10.5194/gmd-2022-182 preprint EN cc-by 2022-08-02

Abstract. This paper investigates the influence of multi-decadal climatic variability on temporal evolution root zone storage capacities (Sr,max) and its implications for streamflow predictions at catchment scale. Through a comprehensive analysis 286 catchments across Europe US, we analyse deviations in evaporative ratios (IE) from expected values based aridity (IA) their subsequent impact Sr,max predictions. Our findings reveal that while do not strictly adhere to specific parametric Budyko...

10.5194/egusphere-2024-115 preprint EN cc-by 2024-02-26

Abstract. This paper investigates the influence of multi-decadal climatic variability on temporal evolution root zone storage capacities (Sr,max) and its implications for streamflow predictions in Meuse basin. Through a comprehensive analysis 286 catchments across Europe US that are hydro-climatically comparable to basin, we construct inter-decadal distributions past deviations evaporative ratios (IE) from expected values based catchment aridity (IA). These ΔIE were then used estimate...

10.5194/hess-28-4577-2024 article EN cc-by Hydrology and earth system sciences 2024-10-23

Abstract. Intercatchment groundwater flows (IGF), defined as across topographic divides, can occur regional that bypass headwater streams and only drain into the channel further downstream or directly to sea. However, also be diverted adjacent river basins due geological features (e.g., faults, dipping beds highly permeable conduits). Even though intercatchment a significant part of water balance, they are often not considered in hydrological studies. Yet, assuming this process negligible...

10.5194/hess-2018-370 preprint EN cc-by 2018-07-09

<p>Models calibrated on the past are often used to predict future hydrological behavior in a changing world, disregarding that systems, hence model parameters, will change as well. Even if we aware of non-stationarity impeded by our limited knowledge how meaningfully implement this models. Yet, ecosystems likely adapt response climate and other species might become dominant, both under natural anthropogenic influence. The root-zone storage capacity is an important parameter,...

10.5194/egusphere-egu21-4058 article EN 2021-03-03

Abstract This paper presents an analysis of future research and development needs to assess the effectiveness nature-based solutions for climate adaptation in watersheds at scale using hydrological models. Two main questions are addressed: what extent model approaches able support decision making on adaptation, how well is this embedded broader planning process? To research, case studies Bhutan, Zimbabwe Netherlands presented. The Climate Risk Informed Decision Analysis approach used...

10.14321/aehm.026.02.019 article EN Aquatic Ecosystem Health & Management 2023-04-01

In this paper, we present a model of hysteresis motor based on Maxwell's equations coupled with the Jiles-Atherton (J-A) solved by finite element method. The aim work is to validate such comparison experimental results (electromagnetic torque, voltage, current). We also an analysis when imposing current or voltage in 2D vector potential formulation.

10.1051/epjap:2004224 article EN The European Physical Journal Applied Physics 2004-12-21

Abstract. International collaboration between research institutes and universities is a promising way to reach consensus on hydrological model development. Although comparative studies are very valuable for international cooperation, they do often not lead clear new insights regarding the relevance of modelled processes. We hypothesise that this partly caused by complexity comparison methods used, which focus too much good overall performance instead focusing specific events. In study, we...

10.5194/hess-2016-339 preprint EN cc-by 2016-07-20

Understanding extreme discharge behavior is of importance for flood design and risk management. For example, estimates large return periods such as the 100-year period or higher are often needed a basis hazard maps dike design. Yet, frequency analysis based on decade-long records show uncertainty these frequencies, among others due to statistical from distribution parameters.  This not case shape parameter, key parameter that describes upward downward curvature tail thus an...

10.5194/egusphere-egu24-16095 preprint EN 2024-03-09

<p>Estimates of water volumes stored in the root-zone vegetation are a key element controlling hydrological response catchment. Remotely-sensed soil moisture products available globally. However, they representative upper-most few centimeters soil. For reliable runoff predictions, we interested estimates as regulate partitioning precipitation to drainage and evaporation. The Soil Water Index approximates from near-surface requires single parameter representing characteristic...

10.5194/egusphere-egu2020-6917 article EN 2020-03-09

<p>The release of the European Centre for Medium-Range Weather Forecasts (ECMWF)’s Re-Analysis 5 (ERA-5) global climate forcing dataset is expected to greatly improve quality hydrological modeling. Following this there great interest in assessing improvements ERA-5 relative its predecessor ERA-Interim modeling and predictions.</p><p>In study we compare streamflow predictions when using ERA-interim vs as data a suite models from...

10.5194/egusphere-egu2020-10219 article EN 2020-03-09
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