气候变化研究进展 ›› 2013, Vol. 9 ›› Issue (3): 173-180.doi: 10.3969/j.issn.1673-1719.2013.03.003

• CMIP5专栏 • 上一篇    下一篇

CMIP5耦合模式对北半球3—4月积雪面积的历史模拟和未来预估

朱献1, 2, 董文杰2   

  1. 1 兰州大学大气科学学院
    2 北京师范大学地表过程与资源生态国家重点实验室
  • 收稿日期:2013-01-28 修回日期:2013-03-25 出版日期:2013-05-30 发布日期:2013-05-30
  • 通讯作者: 朱献 E-mail:zhuxian276@163.com
  • 基金资助:

    全球变化重大科学研究计划

Evaluation and Projection of Northern Hemisphere March-April Snow Covered Area Simulated by CMIP5 Coupled Climate Models

Zhu Xian1, 2, Dong Wenjie2   

  1. 1 College of Atmospheric Sciences, Lanzhou University
    2 State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University
  • Received:2013-01-28 Revised:2013-03-25 Online:2013-05-30 Published:2013-05-30
  • Contact: Xian ZHU E-mail:zhuxian276@163.com

摘要: 基于卫星观测数据,评估了23个CMIP5耦合模式对北半球3—4月积雪面积的模拟能力,在此基础上应用多模式集合平均结果,预估了未来不同温室气体排放情景下北半球3—4月积雪面积的变化情况。结果表明:整体上看,CMIP5耦合模式对北半球3—4月积雪面积具有一定的模拟能力,模式基本能再现北半球3—4月积雪面积的分布特征,但对高原等复杂地形地区积雪的模拟偏差较大并且低估了北半球积雪的减少趋势,这些可能是由卫星资料本身的缺陷以及模式参数化方案的不同造成的。多模式集合预估结果表明,未来几十年北半球3—4月积雪将继续减少并且集中发生在欧亚大陆中西部地区。温室气体排放将会对未来北半球积雪的变化产生显著影响。在RCP8.5情景下,未来北半球积雪减少最显著;在RCP4.5和RCP6.0情景下,在21世纪前半叶北半球积雪减少趋势与RCP8.5情景相当,但是在21世纪后半叶积雪的减少趋势明显小于RCP8.5情景;在RCP2.6情景下,北半球积雪减少趋势最小。所以,控制温室气体排放对于未来北半球积雪的生存至关重要。

关键词: 积雪, CMIP5, 预估

Abstract: Based on the dataset observed by the meteorological satellites from NOAA, the simulated Northern Hemisphere March-April snow cover fraction (SNC) in historical experiments from 23 coupled climate models attending the fifth phase of the Coupled Models for Inter-comparison Project (CMIP5) was evaluated. The 23 models were aggregated by arithmetic mean to project the changes of Northern Hemisphere March-April SNC in 2006-2099. The results show that, overall, the CMIP5 coupled models reproduce the observed snow cover extent well and catch the main characteristics in the distribution of snow cover. But the simulation of snow cover in complex terrain area such as Qinghai-Tibet Plateau is poor and the significant trend towards a reduced spring snow cover extent over 1979-2005 is underestimated. The defect of satellite data and differences of parameterization schemes used in different models may be the causes. The projection by multi-model ensemble show that, the snow cover will continue to reduce in the next few decades mainly in the central and western regions of Eurasia. Greenhouse gas emissions will have a significant impact on the change of Northern Hemisphere snow cover in the future. The northern Hemisphere snow cover will reduce the most significantly under RCP8.5 scenario. Under RCP4.5 and RCP6.0 scenarios, the reduction of snow cover is equivalent to that under RCP8.5 scenario in the first half of the 21st century, but the decreasing trend is significantly less than that under RCP8.5 scenario in the last half of the 21st century. Under RCP2.6 scenario, the reduction of snow cover will not be significant. Therefore, it is crucial to control the discharge of greenhouse gas emissions for mitigating the disappearance of snow cover over Northern Hemisphere.

Key words: snow cover, CMIP5, projection

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