院报 ›› 2024, Vol. 41 ›› Issue (1): 36-43.DOI: 10.11988/ckyyb.20221144

• 水资源 • 上一篇    下一篇

基于CanESM5模式的长江流域未来降雨变化趋势分析

欧阳硕1, 胡智丹2, 邵骏1, 龚莉3, 杜涛1   

  1. 1.长江水利委员会水文局,武汉 430010;
    2.水利部信息中心(水利部水文水资源监测预报中心),北京 100053;
    3.武汉大学 水资源与水电工程科学国家重点实验室,武汉 430072
  • 收稿日期:2022-11-30 修回日期:2023-02-07 出版日期:2024-01-01 发布日期:2024-01-15
  • 作者简介:欧阳硕(1988-),男,湖北监利人,高级工程师,博士,主要从事流域水文水资源、区域水资源配置和水库群优化调度研究。E-mail:Shuo_Ouyang@126.com
  • 基金资助:
    国家重点研发计划项目(2019YFC0408901-02);中国长江三峡集团有限公司资助项目(0711606)

Future Rainfall Change Trend in Yangtze River Basin Based on CanESM5 Model

OUYANG Shuo1, HU Zhi-dan2, SHAO Jun1, GONG Li3, DU Tao1   

  1. 1. Bureau of Hydrology,Changjiang Water Resources Commission,Wuhan 430010, China;
    2. Information Center (Hydrology Monitor and Forecast Center), Ministry of Water Resources, Beijing 100053,China;
    3. State Key Laboratory of Water Resources and Hydropower Engineering Science,Wuhan University,Wuhan 430072,China
  • Received:2022-11-30 Revised:2023-02-07 Online:2024-01-01 Published:2024-01-15

摘要: 长江流域位于我国东部季风区,受气候变化影响明显,频繁而严重的洪旱灾害问题突出,急需开展水文气象要素未来时空变化趋势分析。引入CMIP6发布的CanESM5模式低、中、高强迫(SSP1-2.6、SSP2-4.5、SSP5-8.5)3种不同情景降雨量预估成果,采用基于分位数的日尺度偏差校正统计降尺度方法,研究了未来40 a降雨量时空演变趋势。空间上长江流域多年平均降雨量维持从西北至东南逐渐增加的空间分布格局不变,时间上以关键控制断面屏山、宜昌未来40 a成果为代表,未来屏山、宜昌以上流域的年降雨量均值及极值较历史时期相比明显增大,且高强迫情景下的年降雨量明显大于低强迫情景和中强迫情景;对于低强迫情景和高强迫情景,屏山断面以上流域年降雨量随时间的线性变化显著,而宜昌断面以上流域年降雨量随时间的线性变化不显著;在中强迫情景下,2个断面以上流域年降雨量随时间的线性变化显著。

关键词: 降雨量时空演变趋势, CMIP6, CanESM5模式, 基于分位数的日尺度偏差校正法, 长江流域

Abstract: Situated in the eastern monsoon region of China, Yangtze River Basin is highly vulnerable to the impacts of climate change and prone to be stricken by frequent and severe flood and drought disasters. It is crucial to analyze the future spatiotemporal trends of hydrological and meteorological elements in the Yangtze River Basin. Based on the precipitation prediction results of the CanESM5 model released by CMIP6 under low, medium, and high forcing scenarios, namely SSP1-2.6, SSP2-4.5, and SSP5-8.5, respectively, we employed the daily bias correction method to examine the spatiotemporal evolution of precipitation over the next four decades. In spatial scale, the annual average precipitation across the Yangtze River Basin remains a pattern of increasing from northwest to southeast; and in temporal scale, future precipitation trends in the upstream basins of Pingshan and Yichang, which are key control stations, exhibit significantly higher mean and extreme values over the next four decades than those in historical period. In particular, precipitation levels in the SSP5-8.5 scenario are notably higher than those observed in the SSP1-2.6 and SSP2-4.5 scenarios. Moreover, we observed a significant linear correlation between annual precipitation and time in the upstream of Pingshan section under the SSP1-2.6 and SSP5-8.5 scenarios, but no significant correlation for the Yichang section. However, under the SSP2-4.5 scenario, the correlation between annual precipitation and time in the upstream of both sections remains significant.

Key words: spatiotemporal evolution trend of precipitation, CMIP6, CanESM5 model, quantile-based daily bias correction, Yangtze River Basin

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