气候变化情景下吉尔吉斯跨界河流(锡尔河流域和阿姆河流域)径流评估

O. Kalashnikova, J. Niyazov, Aliya Nurbatsina, S. Kodirov, Yulia Radchenko, Zoya Kretova
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引用次数: 0

摘要

这项研究是吉尔吉斯共和国向《联合国气候变化框架公约》提交的第四次国家信息通报中“水资源”部分的一部分。本文介绍了吉尔吉斯斯坦(锡尔河-达里亚河和阿姆河-达里亚河流域)水资源、气候和冰川长期观测的现状和变化。选取了吉尔吉斯斯坦、乌兹别克斯坦、哈萨克斯坦和塔吉克斯坦的跨界代表性河流作为主要研究对象。基于气候预估CMIP5 (RCP4.5和RCP8.5)和CMIP6 (SSP2-4.5和SSP5-8.5) (IPCC第二工作组报告,2022),评估2020 - 2080年期间河流流量的年际和年内动态。采用HBV light和HBV EHT模型中的水文建模方法和惯性平均年流量变化法估算水资源变化。在费尔干纳河谷北部的河流上,预计年平均径流量将增加1-19%,在Amudarya河流域(kyzil - suu河),预计将增加2006-2019年径流量的27-64%。在纳林河,这一时期的水量将保持在2006-2019年的当前值。平均年径流量的惯性变化方法显示,所有研究的流域在2030年和2040年的径流量增加了当前2006-2020年的6-19%。研究结果可为气候变化条件下水资源的合理利用和长期规划提供参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Kyrgyz transboundary rivers’ runoff assessment (Syr-darya and Amu-darya river basins) in climate change scenarios
The research was carried out as part of the preparation “Water Resources” section of the 4th National Communication of the Kyrgyz Republic to the UNFCCC. The article presents extensive information on the current state and changes over a long period of observations of water resources, climate and glaciation in Kyrgyzstan (Syr-Darya and Amu-Darya river basins). The representative rivers were selected as the main objects, which are transboundary between Kyrgyzstan, Uzbekistan, Kazakhstan and Tajikistan. The study aims to assess the inter-annual and intra-annual dynamics of the flow of the rivers for the period from 2020 to 2080, based on the climate projections CMIP5 (RCP4.5 and RCP8.5) and CMIP6 (SSP2-4.5 and SSP5-8.5) (IPCC WG II Report, 2022). The hydrological modeling method in the HBV light and HBV EHT models and the inertial mean annual flow change method were used to estimate changes in water resources. On the rivers of the northern part of the Fergana Valley, the average annual runoff is expected to increase by 1-19%, in the Amudarya river basin (Kyzyl-Suu river) – by 27-64% of the values for 2006-2019. In the Naryn river, water discharge for this period will remain within the current values for 2006-2019. The method of inertial change in the average annual runoff showed an increase in runoff for 2030 and 2040 for all the studied catchment areas by 6-19% of the current values for 2006-2020. The results of the study are intended for decision-makers on the rational use and long-term planning of water resources under climate change.
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