نوع مقاله : مقاله کامل علمی پژوهشی
نویسندگان
1 دانشجوی کارشناسی ارشد هواشناسی کشاورزی دانشگاه سمنان
2 استادیار گروه بیابانزدایی دانشکده کویرشناسی دانشگاه سمنان
3 استادیار گروه مهندسی آب دانشگاه رازی کرمانشاه
چکیده
کلیدواژه‌ها
عنوان مقاله [English]
نویسندگان [English]
Background and Objectives: The phenomenon of climate change and its impact on water resources is of utmost importance that has been less investigated in our country.In this study, The meteorological variables in terms of predicted climate change and were compared with the present situation. The effect of this phenomenon on Dinavar Kermanshah discharge basin taking into account the uncertainty was evaluated.
Materials and Methods: To this end, results of 6 model coupled atmosphere - ocean general circulation of the atmosphere contains MPEH5, IPCM4, INCM3, HADCM3, GFCM21 and NCCCSM under scenarios of greenhouse gas emissions SRESS includes A1B, A2 and B1 were Downscaling using the LARS-WG software. To determine the accuracy of the models and scenarios, temperature and precipitation observational data were compared with temperature and precipitation available data on Canada base models and scenarios and weighted method was used to evaluate uncertainty models and scenarios. Then, base of scenario and models uncertainty, was predicted variables in coming period (2011-2034) and (2046-2069) compared with the base period (1987-2010). After the downscaling of climate variables, IHACRES rainfall-runoff models used to simulate runoff in future periods.
Results: Based on the results, it's expected that temperature will be increased respectively 1.72 ,1.55 and 1.39 ° C in 2011-2034 and 3.27, 2.88 and 2.26 ° C in 2046-2069, for A1B, A2 and B1 scenarios compared to the baseline in Dinavar basin. As well as precipitation changes respectively has been 15.22, 17.94 and 23.27 mm for A1B, A2 and B1 scenarios in 2011-2034, and -35.4, 7.97 and 2.58 mm for A1B, A2 and B1 scenarios in 2046-2069 compared to the baseline in this basin. The results showed that the amount of average flow and runoff volume has been increased in future periods except A1B scenario (2046-2069). But, flow regime of maximum daily discharges showed that it is adjust in future period. Flow - Frequency curve analysis with different probability showed that it is required to build large reservoirs to water supply in low flow seasons in future periods.
Conclusion: The results showed that the amount of average temperature and precipitation will be increased in future periods. So that the increase of temperature in the second period is more than the first period and increase of precipitation in the first period will be more than the second period. Also the amount of discharges in future period will be increased so that the increase in the first period will be more than the second period, and the volume of runoff in the first period will be more than the second period and in both periods were higher than the base period. But flow regime of maximum daily discharges showed the decreasing in future period, So that the maximum discharge rate decrease in the second period is more than the first period. Flow - Frequency curve analysis also showed that in the absence ofwater storage, agriculture andindustry and drinkingin the area faced withsupply problems.
کلیدواژه‌ها [English]
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