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T.L. Hà

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5 records found

Journal article (2025) - Lan Thanh Ha, W. G.M. Bastiaanssen, Narendra Das, Tim Hessels
Study region: This study covers 16 major river basins across Vietnam, encompassing diverse topographies and climatic zones. These basins represent key regions for national water resource planning, agricultural development, and ecosystem conservation. Study focus: This study presents the quantification results of Hydrological EcoSystem Services (HESS) for 16 major river basins in Vietnam, using integrated earth observation datasets with water and energy balance models such as the Regional Hydrological Extremes for Agriculture System (RHEAS) by NASA-JPL and the Water Productivity (WaPOR) by FAO. Eight HESS indicators, such as total runoff, rootzone water storage, carbon sequestration, and microclimate cooling were evaluated for the hydrological years, representing wet, average, and dry climatic conditions (2005, 2010, 2019 and 2022). A synthesized score was introduced to benchmark sustainability level of these basins throughout the period. New hydrological insights for the region: The results reveal distinct exhibit a diverse distribution of HESS across basins, interrelationship as well as trade-offs. This study illustrates how remote sensing data and spatial algorithms can be applied to determine various aspects of HESS across different landscapes and ecosystems. Basins in the central regions exhibited stronger ecosystem performance, while those in the more urbanized northern and southern regions showed comparatively lower levels. With quantified HESS and benchmarked sustainability score, the natural capital assets of Vietnam are herewith revealed, and this system can also be applied to other countries. The findings underscore the value of integrating earth observation and ecohydrological modelling to support HESS monitoring, the design of Nature-based Solutions (NbS), and sustainable water resource planning in data-scarce regions. ...
Doctoral thesis (2025) - T.L. Hà, W.G.M. Bastiaanssen, G.H.W. Schoups
Hydrological ecosystem services (HESS), also referred to as water-related ecosystem services, highlight the intricate connection between ecosystem services and the hydrological cycle. This relationship underscores that the magnitude of these services is largely dependent on the availability and quality of water. The inclusion of HESS ensures the transition from traditional top-down and single objective systems into multi-criteria and human-centered approaches that can prioritize activities with a broader spectrum of benefits. In particular, HESS ensures the uptake of international guidance, such as Integrated Water Resources Management (IWRM), Nature-based Solutions (NbS) or Natural Capital Accounting (NCA), by achieving a win-win co-development of water with, among others, land and ecosystems, while fully delivering the benefits to humans and society. ...
Journal article (2023) - Lan Thanh Ha, Wim G. M. Bastiaanssen, Gijs W. H. Simons, Ate Poortinga
Hydrological ecosystem services (HESS) describe the benefits of water for multiple purposes with an emphasis on environmental values. The value of HESS is often not realized because primary benefits (e.g., food production, water withdrawals) get the most attention. Secondary benefits such as water storage, purification or midday temperature cooling are often overlooked. This results in an incorrect evaluation of beneficial water usage in urban and rural resettlements and misunderstandings when land use changes are introduced. The objective of this paper is to propose a standard list of 17 HESS indicators that are in line with the policy and philosophy of the Consultative Group of International Agricultural Research (CGIAR) and that are measurable with earth observation technologies in conjunction with GIS and hydrological models. The HESS17 framework considered indicators that can be directly related to water flows, water fluxes and water stocks; they have a natural characteristic with minimal anthropogenic influence and must be quantifiable by means of earth observation models in combination with GIS and hydrological models. The introduction of a HESS framework is less meaningful without proper quantification procedures in place. Because of the widely diverging management options, the role of water should be categorized as (i) consumptive use (i.e., evapotranspiration and dry matter production) and (ii) non-consumptive use (stream flow, recharge, water storage). Governments and responsible agencies for integrated water management should recognize the need to include HESS17 in water allocation policies, water foot-printing, water accounting, transboundary water management, food security purposes and spatial land-use planning processes. The proposed HESS17 framework and associated methods can be used to evaluate land, soil and water conservation programs. This paper presents a framework that is non-exhaustive but can be realistically computed and applicable across spatial scales. ...
Journal article (2023) - Lan Thanh Ha, Wim G. M. Bastiaanssen
The principles of Integrated Water Resources Management (IWRM), conservation of natural capital, and water accounting requires Hydrological Eco-System Services (HESS) to be determined. This paper presents a modeling approach for quantifying the HESS framework using the Soil Water Assessment Tool (SWAT). SWAT was used–after calibration against remote sensing data–to quantify and spatially identify total runoff, natural livestock feed production, fuelwood from natural forests, dry season flow, groundwater recharge, root zone storage for carrying over water from wet to dry season, sustaining rainfall, peak flow attenuation, carbon sequestration, microclimate cooling, and meeting environmental flow requirements. The environmental value of the current land use and vegetation was made explicit by carrying out parallel simulations for bare soil and vegetation conditions and reporting the incremental ecosystem services. Geographical areas with more and fewer HESS are identified. The spatial and temporal variability of annual HESS services is demonstrated for the Day Basin—which is part of the Red River delta (Vietnam)—for the period 2003 to 2013. The result shows that even though the basin is abundant with HESS, e.g., 7482 m3/ha of runoff, 3820 m3/ha of groundwater recharge, the trend for many HESS values, e.g., micro-climate cooling, meeting environmental flow requirements, and rootzone storage, are declining. It is found and proven that quantified HESS indicators highlighted the provisioning and regulating characters of ecosystem services, as well as geographical hotspots across the basin. The SWAT model shows the capability of simulating terrestrial eco-hydrological processes such as climate, soil, and current land use. The methodology illustrates how eco-hydrologists can benchmark ecosystem values and include HESS in exploring river basin management scenarios, climate change studies, and land use planning. ...
Journal article (2018) - Lân Hà, Wim G.M. Bastiaanssen, Ann van Griensven, Albert I. .J M. van Dijk, Gabriel B. Senay
In this paper, evapotranspiration (ET) and leaf area index (LAI) were used to calibrate the SWAT model, whereas remotely sensed precipitation and other climatic parameters were used as forcing data for the 6300 km2 Day Basin, a tributary of the Red River in Vietnam. The efficacy of the Sequential Uncertainty Fitting (SUFI-2) parameter sensitivity and optimization model was tested with area specific remote sensing input parameters for every Hydrological Response Units (HRU), rather than with measurements of river flow representing a large set of HRUs, i.e., a bulk calibration. Simulated monthly ET correlations with remote sensing estimates showed an R2 = 0.71, Nash-Sutcliffe Efficiency NSE = 0.65, and Kling Gupta Efficiency KGE = 0.80 while monthly LAI showed correlations of R2 = 0.59, NSE = 0.57 and KGE = 0.83 over a five-year validation period. Accumulated modelled ET over the 5-year calibration period amounted to 5713 mm compared to 6015 mm of remotely sensed ET, yielding a difference of 302 mm (5.3%). The monthly flow at two flow measurement stations were adequately estimated (R2 = 0.78 and 0.55, NSE = 0.71 and 0.63, KGE = 0.59 and 0.75 for Phu Ly and Ninh Binh, respectively). This outcome demonstrates the capability of SWAT model to obtain spatial and accurate simulation of eco-hydrological processes, also when rivers are ungauged and the water withdrawal system is complex. ...