中国科学技术大学学报 ›› 2020, Vol. 50 ›› Issue (7): 1003-1012.DOI: 10.3969/j.issn.0253-2778.2020.07.018

• 论著 • 上一篇    下一篇

RCP8.5情景下长江中下游降水变化预估不确定性

孔海妹,李根,孙亮   

  1. 1.中国科学技术大学地球和空间科学学院,安徽合肥 230026;2.武汉中心气象台,湖北武汉 430074;
  • 收稿日期:2020-02-25 修回日期:2020-04-29 接受日期:2020-04-29 出版日期:2020-07-31 发布日期:2020-04-29
  • 通讯作者: 李根
  • 作者简介:孔海妹,女,1995年生,硕士. 研究方向:气候变化. E-mail:hm199568@mail.ustc.edu.cn
  • 基金资助:
    国家自然科学基金(41876013), “全球变化与海气相互作用”专项国际合作项目(GASI-IPOVAI-04)资助.

The uncertainty of projection of precipitation change in the middle and lower reaches of the Yangtze River under the RCP8.5 scenario

KONG Haimei, LI Gen, SUN Liang   

  1. 1.School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China; 2.Wuhan Central Meteorological Observatory, Wuhan 430074, China;
  • Received:2020-02-25 Revised:2020-04-29 Accepted:2020-04-29 Online:2020-07-31 Published:2020-04-29

摘要: 利用第五次耦合模式比较计划(CMIP5)的历史模拟以及典型浓度路径(RCP8.5)高排放情景下的实验资料,对全球变暖下长江中下游夏季的降水变化进行了预估.结果表明,多模式平均预估的全球变暖下长江中下游降水变化增加幅度较小.一方面全球变暖导致水汽含量增加,有利于长江中下游降水增加;另一方面,全球变暖下夏季风环流减弱,不利于长江中下游降水增加.两者共同作用下,多模式平均预估的长江中下游未来夏季降水变化不明显.这一预估结果存在很大的模式间不确定性.分析表明,模式对降水变化预估的不确定性主要来源于大尺度夏季风环流变化预估的不确定性,而气候变暖所致的水汽增加对降水变化不确定性的影响较小.对这种不确定性来源的进一步研究表明,长江中下游降水及东亚夏季风环流变化均与北大西洋和西北太平洋海温增暖幅度相关,北大西洋海温影响更显著.这说明,在全球强增暖背景下北大西洋和西北太平洋海温增暖对长江中下游降水变化预估有很大的影响,如果能降低两个区域海温变化预估的不确定性,长江中下游降水预估结果将更为可靠.

关键词: 全球变暖, 长江中下游, 降水, CMIP5

Abstract: Summer precipitation changes in the middle and lower reaches of the Yangtze River under global were estimated, using the historical simulation of the fifth coupled mode comparison plan (CMIP5) and the experimental data under the high concentration scenario of the typical concentration path (RCP8.5). The results show that the multi-mode average predicted global warming has a small increase in precipitation variation in the middle and lower reaches of the Yangtze River. On the one hand, global warming leads to an increase in water vapor content, which is conducive to the increase of precipitation in the Yangtze River Basin. On the other hand, global warming has caused the Summer monsoon circulation to weaken, and the weakened summer monsoon is not conducive to the increase of precipitation in the Yangtze River basin. Under the combined effect of the two, the multi-model average estimated mid-downstream watershed in the Yangtze River has no obvious changes in summer precipitation. However, there is a large inter-mode uncertainty in this estimate. The analysis shows that the uncertainty of the prediction of precipitation change is mainly due to the uncertainty of precipitation prediction results caused by large-scale Summer monsoon circulation changes, and the increase of water vapor caused by climate warming has less influence on the uncertainty of precipitation variation. Further research on this source of uncertainty shows that precipitation in the middle and lower reaches of the Yangtze River and changes in the East Asian summer monsoon circulation are strongly correlated with the warming of the North Atlantic and the the Western North Pacific SST. This indicates that in the context of global warming, the warming of the North Atlantic and the Western North Pacific SST has a great impact on the prediction of precipitation changes in the middle and lower reaches of the Yangtze River. If the uncertainty of the prediction of the North Atlantic and the Western North Pacific SST is reduced, the precipitation prediction results in the middle and lower reaches of the Yangtze River will be more reliable.

Key words: global warming, middle and lower reaches of the Yangtze River, precipitation, CMIP5

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