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Projecting the climate change impact on water yield in a cold mountainous watershed, Ardabil | ||
| فیزیک زمین و فضا | ||
| مقالات آماده انتشار، پذیرفته شده، انتشار آنلاین از تاریخ 15 دی 1403 اصل مقاله (807.75 K) | ||
| نوع مقاله: مقاله پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22059/jesphys.2025.375570.1007601 | ||
| نویسندگان | ||
| ابراهیم عسگری1؛ رئوف مصطفی‌زاده* 2؛ حسین طالبی خیاوی3 | ||
| 1دکتری علوم و مهندسی آبخیزداری، گروه مهندسی آبخیزداری، دانشکده منابع طبیعی و کویرشناسی، دانشگاه یزد، یزد، ایران | ||
| 2دانشیار گروه منابع طبیعی و عضو پژوهشکده مدیریت آب، دانشکده کشاورزی و منابع طبیعی، دانشگاه محقق اردبیلی | ||
| 3دانشجوی دکتری علوم جغرافیایی، موسسه جغرافیا، آکادمی علوم اسلوواک، براتیسلاوا، اسلواکی | ||
| چکیده | ||
| Population growth and climate change are worsening pressure on water supplies, altering rainfall-runoff patterns, and posing significant challenges for water management. Climate change profoundly affects society, particularly water reserves, through temperature shifts, precipitation changes, and disruptions to river flows, ultimately impacting water scarcity and ecosystem services. The objective of this study is to project the possible effects of climate change on water yield in a cold-climate watershed located in Ardabil province. The GR4J conceptual model used to simulate the hydrologic watershed response to changes in climatic factors. The HadCM3 model, was used to examine meteorological parameters under the A1B climate scenario through implementing LARS-WG. The GR4J has been calibrated using trial-and-error method to maximize the NS coefficient. he validation results were evaluated using NS and RE. The results showed a significant variation in water yield values across different periods. The highest yearly water yield is in 2030, dropping to 49.79 million cubic meters in 2050, representing a 13.6 million cubic meters decrease. Based on the results, the highest positive change occurred in February, where the percentage increased from 93% in 2030 to 138% in 2060, representing a 45% increase. Additionally, the highest negative change is projected in October, where the percentage decreased from 27% in 2030 to -11% in 2060, representing a decrease of -38%. The results suggests that flood and extreme flow events will increase, while low flow events will decrease significantly under climate change conditions, and the simulated flow values also show more fluctuations in the projected periods. | ||
| کلیدواژه‌ها | ||
| Water Balance؛ Watershed response؛ River flow discharge؛ Climatic variables؛ Environmental Management | ||
| عنوان مقاله [English] | ||
| Projecting the climate change impact on water yield in a cold mountainous watershed, Ardabil | ||
| نویسندگان [English] | ||
| Ebrahim Asgari1؛ Raoof Mostafazadeh2؛ Hossein Talebi Khiavi3 | ||
| 1Ph.D Student in Watershed Management Engineering and Sciences, Department of Watershed Management, Faculty of Natural Resources and Desert Studies, Yazd University, Yazd, Iran | ||
| 2Associate Professor and Member of Water Management Research Center, Department of Natural Resources, Faculty of Agriculture and Natural Resources, University of Mohaghegh Ardabili, Ardabil, Iran | ||
| 3Ph.D Student in Geography, Institute of Geography, Slovak Academy of Sciences, Bratislava, Slovakia | ||
| چکیده [English] | ||
| Population growth and climate change are worsening pressure on water supplies, altering rainfall-runoff patterns, and posing significant challenges for water management. Climate change profoundly affects society, particularly water reserves, through temperature shifts, precipitation changes, and disruptions to river flows, ultimately impacting water scarcity and ecosystem services. The objective of this study is to project the possible effects of climate change on water yield in a cold-climate watershed located in Ardabil province. The GR4J conceptual model used to simulate the hydrologic watershed response to changes in climatic factors. The HadCM3 model, was used to examine meteorological parameters under the A1B climate scenario through implementing LARS-WG. The GR4J has been calibrated using trial-and-error method to maximize the NS coefficient. he validation results were evaluated using NS and RE. The results showed a significant variation in water yield values across different periods. The highest yearly water yield is in 2030, dropping to 49.79 million cubic meters in 2050, representing a 13.6 million cubic meters decrease. Based on the results, the highest positive change occurred in February, where the percentage increased from 93% in 2030 to 138% in 2060, representing a 45% increase. Additionally, the highest negative change is projected in October, where the percentage decreased from 27% in 2030 to -11% in 2060, representing a decrease of -38%. The results suggests that flood and extreme flow events will increase, while low flow events will decrease significantly under climate change conditions, and the simulated flow values also show more fluctuations in the projected periods. | ||
| کلیدواژه‌ها [English] | ||
| Water Balance, Watershed response, River flow discharge, Climatic variables, Environmental Management | ||
| مراجع | ||
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آمار تعداد مشاهده مقاله: 106 تعداد دریافت فایل اصل مقاله: 76 |
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