气候变化情景下干旱半干旱流域水资源配置管理方法研究(研究区:伊朗hablehoud流域)

IF 5.7 3区 环境科学与生态学 Q1 WATER RESOURCES
Morteza Lotfirad, Maral Mahmoudi, Hassan Esmaeili-Gisavandani, Arash Adib
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引用次数: 0

摘要

本文采用低空雷达服务-天气发生器(LARS-WG)模式对由23个大气环流模式(GCMs)输出组成的混合模式进行了统计缩比。此外,为了模拟hablehoud流域(伊朗北部干旱流域)基期(1985 - 2005年)和未来期(2025 - 2045年)的径流,对土壤和水评估工具(SWAT)分布式水文模型进行了校准。针对hablehoud流域2种气候情景(代表性浓度路径(RCP)4.5和RCP8.5)和3种管理情景(S0(基期状态延续)、SI(在不开发水源的情况下增加需水量)和SII(随着宁罗德大坝的建设而增加需水量)下的水资源管理,采用了水资源评价与规划(WEAP)模型。RCP4.5和RCP8.5情景均预测年平均最低(Tmin)和最高(Tmax)温度、降水(PCP)和径流增加。RCP8.5增加幅度更大:Tmin增加1.12°C, Tmax增加1.21°C, PCP增加12.6%,径流增加11.6%。RCP4.5增加幅度较小:Tmin增加0.78°C, Tmax增加0.94°C, PCP增加11.5%,径流量增加6.4%。在这两种气候变化情景下,只要每年增加2%的用水需求,该地区的所有需求都可以在不开发水库的情况下得到满足。在需水量年增长5%的情况下,仅通过水库运行即可满足该地区的需求,但在需水量年增长8%的情况下,该地区的很大一部分需求无法满足。在RCP8.5和RCP4.5情景下,2045年水库运行时的未满足水量分别为136和277 MCM。如果不使用储层,这些值将增加到172和295 MCM。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Allocation of water resources with management approaches and under climate change scenarios in an arid and semi-arid watershed (study area: Hablehroud watershed in Iran)

In this research, the hybrid model consisting of output of 23 general circulation models (GCMs) was statistically downscaled using the lower airspace radar service- weather generator (LARS-WG) model. Also, soil and water assessment tool (SWAT) distributed hydrological model was calibrated in order to simulate the runoff of the Hablehroud basin (an arid watershed in the north of Iran) in the base period (1985 to 2005) and the runoff of the future period (2025 to 2045). To water resources management in the Hablehroud basin under two climate scenarios (representative concentration pathway (RCP)4.5 and RCP8.5) and three management scenarios including, S0 (continuation of the status of the base period), SI (increasing the water demands without development of water supply sources) and SII (increasing water demands with the construction of the Nimrod Dam), the water evaluation and planning (WEAP) model was used. Both RCP4.5 and RCP8.5 scenarios project increases in mean annual minimum (Tmin) and maximum (Tmax) temperatures, precipitation (PCP), and runoff. RCP8.5 shows larger increases: Tmin by 1.12°C, Tmax by 1.21°C, PCP by 12.6%, and runoff by 11.6%. RCP4.5 projects smaller increases: Tmin by 0.78°C, Tmax by 0.94°C, PCP by 11.5%, and runoff by 6.4%. In both scenarios of climate change, with a 2% annual increase in water demand, all the needs of the region can be met without the need to exploit the reservoir. With an annual increase in water demand of 5%, the needs of the region can be met only by operating the reservoir, but with an annual increase of 8% in water demand, a large part of the need of the region cannot be met. The values of unmet water demand in 2045 with operating the reservoir are 136 and 277 MCM under RCP8.5 and RCP4.5 scenarios, respectively. Without using of the reservoir, these values will increase to 172 and 295 MCM.

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来源期刊
Applied Water Science
Applied Water Science WATER RESOURCES-
CiteScore
9.90
自引率
3.60%
发文量
268
审稿时长
13 weeks
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