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مدل‌سازی جریان خروجی زیرحوضه های کارون بزرگ در شرایط اقلیمی آینده | ||
| اکوهیدرولوژی | ||
| مقاله 9، دوره 4، شماره 4، دی 1396، صفحه 1033-1047 اصل مقاله (1.12 M) | ||
| نوع مقاله: پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22059/ije.2017.229255.502 | ||
| نویسندگان | ||
| مرضیه کیهان‌پناه1؛ رفعت زارع بیدکی* 2؛ جواد بذرافشان3 | ||
| 1دانش آموختۀ علوم و مهندسی آبخیزداری، دانشگاه شهرکرد | ||
| 2استادیار دانشکدۀ منابع طبیعی و علوم زمین، دانشگاه شهرکرد | ||
| 3دانشیار دانشکدۀ مهندسی و فناوری کشاورزی، دانشگاه تهران | ||
| چکیده | ||
| تغییر اقلیم با تغییر در چرخۀ هیدرولوژی، جریان خروجی از حوضه را تحت تأثیر قرار میدهد. دانستن میزان تغییرات احتمالی در مقادیر بارش و رواناب خروجی حوضه به برنامهریزی و مدیریت بهتر منابع آب کمک خواهد کرد. تغییرات بارش ناشی از تغییر اقلیم با مدلهای گردش عمومی جوّ تحت سناریوهای مختلف شبیه‌سازی میشود. بررسی تغییرات رواناب به کاربرد مدلهای بارش‌ـ رواناب نیاز دارد. هدف از این پژوهش، مدل‌سازی جریان خروجی بخشی از حوضۀ کارون، که از تغییر اقلیم به‌وجود آمده، است. بنابراین، دما و بارش حوضۀ آبخیز کارون بزرگ برای سالهای 2011 تا 2030 و 2046 تا 2065، با استفاده از دو مدل گردش عمومی جوّ و فرایند کوچک‌مقیاس‌سازی تحت دو سناریوی A2 و B1 شبیه‌سازی شد. سپس جریان خروجی سه زیرحوضۀ اندیمشک، اهواز و یاسوج بهوسیلۀ مدل بارش رواناب IHACRES و با استفاده از مقادیر بارش و دمای پیشبینیشده تحت دو سناریوی A2 و B1 شبیه‌سازی شد. مقایسه‌ها نشان داد در دورههای آتی تحت هر دو سناریو، مقادیر بارش، بیشترین و کمترین دما افزایش خواهند داشت. نتایج شبیه‌سازی رواناب نیز نشان داد در حوضههای مطالعه‌شده میزان رواناب دورههای آتی تحت هر دو سناریو، در فصلهای بهار و تابستان، کاهش و در پاییز و زمستان، افزایش خواهد یافت. | ||
| کلیدواژه‌ها | ||
| پیشیابی؛ تغییر اقلیم؛ شبیه‌سازی؛ کوچک‌مقیاس‌سازی آماری؛ مدل چرخش عمومی جوّ | ||
| عنوان مقاله [English] | ||
| Flow Modelling in Great Karun Sub-basins in terms of Future Climate | ||
| نویسندگان [English] | ||
| Marziyeh kayhanpanah1؛ Rafat Zare Bidaki2؛ Javad Bazrafshan3 | ||
| 1M.Sc. in Watershed Management Science and Engineering, Shahrekord University, Shahrekord, Iran | ||
| 2Assistant Professor, Department of Rangeland and Watershed Management, Shahrekord University, Shahrekord, Iran | ||
| 3Associate Professor, Faculty of Agricultural Engineering and Technology, Tehran University, Tehran, Iran | ||
| چکیده [English] | ||
| Climate change affects runoff flow of the basin by changing in hydrological cycle parameters. Knowing the possible changes in the amount of precipitation and runoff of the basin will help to better planning and management of water resources. Precipitation changes due to climate change can be simulated using atmospheric general circulation models under different scenarios. Assessment of runoff needs using precipitation- runoff models. The aim of this research is flow modelling in some parts of the Great Karun Basin as a result of possible changes in future climate. For this purpose, temperature and precipitation changes of the Great Karun Basin are simulated for years 2011-2030 and 2046-2065 using two general circulation models and downscaling process under B1 and A2 scenarios. Then, the output flow of Andimeshk, Ahwaz and Yasouj sub-basins was predicted by IHACRES rainfall- runoff model and using precipitation and temperature data predicted under B1 and A2 scenarios. Compare revealed that, the amount of precipitation, maximum temperature and minimum temperature will increase in future periods under both scenarios. The results of flow simulation also show that the runoff of future periods under both scenarios will decrease in spring and summer and increase in autumn and winter in study area. | ||
| کلیدواژه‌ها [English] | ||
| climate change, simulation, General Atmospheric circulation Model, Statistical Downscaling | ||
| مراجع | ||
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