Effects of Climate Change and Changes in Land Use and Cover on Water Yield in an Equatorial Andean Basin DOI Creative Commons
Darío Zhiña, Álex Avilés,

Lorena González

et al.

Hydrology, Journal Year: 2024, Volume and Issue: 11(9), P. 157 - 157

Published: Sept. 23, 2024

Ecosystem services contribute significantly to human development, with water production being a crucial component. Climate and land use changes can impact availability within basin. In this context, researching water-related areas is essential for formulating policies protect manage hydrological services. The objective of study was estimate yield in the sub-basins Tabacay Aguilán rivers under climate change scenarios 2030, 2040, 2050, combined cover use. InVEST model employed analyze yield. results show that crop were identified as lowest future scenarios, forested areas, particularly region where Cubilán Protected Forest located, most subbasin. Besides, has increased historic period (2016–2018) due conservation reforestation initiatives carried out by Municipal Public Service Company Drinking Water, Sewerage, Environmental Sanitation city Azogues 2018, so-called Reciprocal Agreements Water. Additionally, an increase projected scenarios. This serve basis decision-makers identify should prioritize protection conservation.

Language: Английский

Hybrid molecular fuzzy recommender systems for impact of climate change on renewable energy performance DOI
Yedan Shen, Wei Liu, Hasan Dınçer

et al.

Renewable Energy, Journal Year: 2025, Volume and Issue: unknown, P. 122799 - 122799

Published: March 1, 2025

Language: Английский

Citations

1
Assessment of renewable water in the face of climate change by a comprehensive analysis of adaptation strategies DOI
Mohsen Kalantari, Mohammad Reza Nikoo, Nasser Talebbeydokhti

et al.

Climatic Change, Journal Year: 2025, Volume and Issue: 178(3)

Published: March 1, 2025

Language: Английский

Citations

1
Impacts of Extreme Climate on the Water Resource System in Sichuan Province DOI Open Access

Ma Fang,

Zhi Jun Li

Water, Journal Year: 2024, Volume and Issue: 16(9), P. 1217 - 1217

Published: April 24, 2024

Based on the data of Sichuan Province from 2007 to 2021, extreme climate events in was identified by statistical method, and coupling coordination degree water resources-climate system separate resource analyzed. difference under these two systems, influence mechanism factors is The results show that types gradually transition drought precipitation low temperature high temperature. When are not considered, generally improved distribution more concentrated. Moreover, a simple linear relationship.

Language: Английский

Citations

4
Hydrogeological Assessment and Steady-State Groundwater Flow Modeling for Groundwater Management in the Golina River Sub-Basin, Northern Ethiopia, Using MODFLOW 6 DOI Open Access

Hindeya Gebru,

Tesfamichael Gebreyohannes,

Ermias Hagos

et al.

Water, Journal Year: 2025, Volume and Issue: 17(7), P. 949 - 949

Published: March 25, 2025

Unsustainable groundwater extraction for domestic and agricultural purposes, particularly crop irrigation, is leading to dramatic reductions in the quantity quality of many developing countries, including Ethiopia. Assessing predicting responses hydraulic stress caused by overexploitation related anthropogenic activities climate change are crucial informing water management decisions. The aim this study develop a three-dimensional steady-state flow model Golina River Sub-Basin understand relationship between recharge pumping their impacts under conditions from perspective management. was created using MODFLOW 6 discretized into 345 rows 444 columns with grid resolution 100 m m. subsurface modeled as two layers: clastic alluvial layer overlying weathered fractured bedrock. surface-water divide treated no-flow boundary. initial values horizontal conductivity ranged 0.001 m/day rhyolite 27.26 deposits. aquifer rates WetSpass 1.08 × 10−3 2.25 10−4 m/day, discharge springs, hand-dug wells, boreholes were 2.79 104 m3/day, known flux boundaries. Sensitivity analysis revealed that very sensitive conductivity, moderately recharge, less pumping. Calibration performed match observed simulated heads selected wells achieved correlation coefficient 0.998. calibrated 1.2 20 gravel-dominated direction toward southeast, balance indicates negligible difference total (207,775.8297 which entering system) pumped volume (207,775.9373 leaving system). scenario showed an increase rate 25%, 50%, 75% would result decrease head 4.64 m, 10.18 17.38 respectively. A instead hydraulic-head declines 15.29 46.97 Consequently, findings suggest decision-makers should prioritize enhancing integrated strategies improve within system area.

Language: Английский

Citations

0
Effects of Climate Change and Changes in Land Use and Cover on Water Yield in an Equatorial Andean Basin DOI Creative Commons
Darío Zhiña, Álex Avilés,

Lorena González

et al.

Hydrology, Journal Year: 2024, Volume and Issue: 11(9), P. 157 - 157

Published: Sept. 23, 2024

Ecosystem services contribute significantly to human development, with water production being a crucial component. Climate and land use changes can impact availability within basin. In this context, researching water-related areas is essential for formulating policies protect manage hydrological services. The objective of study was estimate yield in the sub-basins Tabacay Aguilán rivers under climate change scenarios 2030, 2040, 2050, combined cover use. InVEST model employed analyze yield. results show that crop were identified as lowest future scenarios, forested areas, particularly region where Cubilán Protected Forest located, most subbasin. Besides, has increased historic period (2016–2018) due conservation reforestation initiatives carried out by Municipal Public Service Company Drinking Water, Sewerage, Environmental Sanitation city Azogues 2018, so-called Reciprocal Agreements Water. Additionally, an increase projected scenarios. This serve basis decision-makers identify should prioritize protection conservation.

Language: Английский

Citations

0