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使用SDSM和CMIP6模型评估气候变化对因陀罗瓦蒂河流域气象变量的影响。

Assessment of climate change impact on meteorological variables of Indravati River Basin using SDSM and CMIP6 models.

作者信息

Challa Venkateswarlu, Renganathan Manjula

机构信息

Department of Civil Engineering, National Institute of Technology, Tiruchirappalli, Tamil Nadu, India.

出版信息

Environ Monit Assess. 2024 Dec 4;197(1):22. doi: 10.1007/s10661-024-13467-4.

Abstract

Climate change, one of the most pressing issues of the twenty-first century, threatens the long-term stability and short-term variability of water resources. Variations in precipitation and temperature will influence runoff and water availability, creating significant challenges as demand for potable water increases. This study addresses a critical literature gap by employing the Statistical Downscaling Model (SDSM) to downscale Global Climate Model (GCM) outputs for the Indravati River Basin, India. Maximum temperature (T), minimum temperature (T), and precipitation (PCP) were statistically downscaled, improving the spatial resolution of coarse GCM data. The model established strong predictor-predictand relationships, offering enhanced local-scale climate projections for the basin. This work provides critical insights into regional climate change impacts in a previously underexplored area. The study projected the meteorological variables (T, T, and PCP) for Chindnar, Jagdalpur, and Pathagudem stations using four GCMs, namely CanESM5, MPI-ESM1-2-HR, EC-Earth3, and NorESM2-LM for the baseline period (1990-2014). The Correlation Coefficient-values (R-values) range from 0.75 to 0.91 for maximum temperature, 0.85 to 0.96 for minimum temperature, and 0.71 to 0.83 for precipitation were achieved using SDSM. The best-performed MPI-ESM1-2-HR model was used to project maximum temperature, minimum temperature, and precipitation for 2024-2054 (2040s) and 2055-2085 (2070s) under SSP4.5 and SSP8.5 scenarios using SDSM. The downscaled results revealed significant shifts in meteorological patterns, highlighting the basin's sensitivity to different socio-economic pathways and future climate conditions. The percentage monthly, seasonal, and annual variations of T, T, and PCP were analysed based on each scenario and time period to suggest remedial measures for future floods and droughts.

摘要

气候变化是21世纪最紧迫的问题之一,它威胁着水资源的长期稳定性和短期变异性。降水和温度的变化将影响径流和水资源的可利用性,随着对饮用水需求的增加,这带来了重大挑战。本研究通过运用统计降尺度模型(SDSM)对印度因德腊瓦蒂河流域的全球气候模型(GCM)输出进行降尺度,填补了关键的文献空白。对最高温度(T)、最低温度(T)和降水量(PCP)进行了统计降尺度,提高了粗糙的GCM数据的空间分辨率。该模型建立了强大的预测因子与预测对象的关系,为该流域提供了增强的局地尺度气候预测。这项工作为一个此前未充分探索的地区的区域气候变化影响提供了关键见解。该研究使用四个GCM,即CanESM5、MPI-ESM1-2-HR、EC-Earth3和NorESM2-LM,对基线期(1990 - 2014年)钦德纳、贾格德尔布尔和帕塔古德姆站点的气象变量(T、T和PCP)进行了预测。使用SDSM得到的相关系数值(R值),最高温度范围为0.75至0.91,最低温度为0.85至0.96,降水量为0.71至0.83。表现最佳的MPI-ESM1-2-HR模型被用于通过SDSM预测2024 - 2054年(2040年代)和2055 - 2085年(2070年代)在SSP4.5和SSP8.5情景下的最高温度、最低温度和降水量。降尺度结果揭示了气象模式的显著变化,突出了该流域对不同社会经济路径和未来气候条件的敏感性。基于每个情景和时间段,分析了T、T和PCP的月度、季节和年度变化百分比,以提出应对未来洪水和干旱的补救措施。

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