AbstractThe main objective of this research is to study the hydrological variabilities by using surface and groundwater coupled model. On that Taiwan is labeled as mountainous watershed with accompanying heavy rains occurred frequently, it is important to understand better the water flow conditions after extreme event occurred. The particular geology and highly concentrated river system could provide more infiltration and percolation of rainwater from surface or streams through permeable soils into water-holding rocks. It may provide useful water supply to undergrounds. In order to study the possible water storage underground in PingTung Plain, we used WASH123D watershed model to study this issue. The WASH123D numerical model is a physical ...
Typhoon-induced flood and inundation are among the major natural disasters in Taiwan. To understand ...
Land subsidence resulting from the overexploitation of groundwater is an important issue in the Chos...
Quantifying the spatiotemporal variations of basin-scale surface water (SW)–groundwater (GW) interac...
AbstractThe main objective of this research is to study the hydrological variabilities by using surf...
This is the final version. Available on open access from Elsevier via the DOI in this recordStudy re...
Groundwater, a salient water resource in Taiwan, has been subject to incessant and excessive pumping...
Abstract The Pingtung Plain is one of the most important groundwater-resource areas in southwestern ...
[[abstract]]In Taiwan, groundwater commonly becomes important water resources in dry periods, and/or...
[[abstract]]Due to nonuniform rainfall distribution in Taiwan, groundwater is an important water sou...
Overexploitation of groundwater is a common problem in the Pingtung Plain area of Taiwan, resulting ...
This study presents the development of an integrated surface and subsurface model for transient anal...
AbstractHualian River is abundant in runoff and high in sediment transport capacity. Most surface wa...
[[abstract]]Groundwater over-exploitation has produced many critical problems in the southern Taiwan...
Interflow is an important water source contributing to river flow. It directly influences the near-s...
The understanding of hydrogeological characteristics and groundwater flow processes in aquifers is c...
Typhoon-induced flood and inundation are among the major natural disasters in Taiwan. To understand ...
Land subsidence resulting from the overexploitation of groundwater is an important issue in the Chos...
Quantifying the spatiotemporal variations of basin-scale surface water (SW)–groundwater (GW) interac...
AbstractThe main objective of this research is to study the hydrological variabilities by using surf...
This is the final version. Available on open access from Elsevier via the DOI in this recordStudy re...
Groundwater, a salient water resource in Taiwan, has been subject to incessant and excessive pumping...
Abstract The Pingtung Plain is one of the most important groundwater-resource areas in southwestern ...
[[abstract]]In Taiwan, groundwater commonly becomes important water resources in dry periods, and/or...
[[abstract]]Due to nonuniform rainfall distribution in Taiwan, groundwater is an important water sou...
Overexploitation of groundwater is a common problem in the Pingtung Plain area of Taiwan, resulting ...
This study presents the development of an integrated surface and subsurface model for transient anal...
AbstractHualian River is abundant in runoff and high in sediment transport capacity. Most surface wa...
[[abstract]]Groundwater over-exploitation has produced many critical problems in the southern Taiwan...
Interflow is an important water source contributing to river flow. It directly influences the near-s...
The understanding of hydrogeological characteristics and groundwater flow processes in aquifers is c...
Typhoon-induced flood and inundation are among the major natural disasters in Taiwan. To understand ...
Land subsidence resulting from the overexploitation of groundwater is an important issue in the Chos...
Quantifying the spatiotemporal variations of basin-scale surface water (SW)–groundwater (GW) interac...