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未来50a中国地区冻土面积分布变化
引用本文:王澄海,靳双龙,施红霞. 未来50a中国地区冻土面积分布变化[J]. 冰川冻土, 2014, 36(1): 1-8. DOI: 10.7522/j.issn.1000-0240.2014.0001
作者姓名:王澄海  靳双龙  施红霞
作者单位:1. 兰州大学 大气科学学院/甘肃省干旱气候变化与减灾重点实验室, 甘肃 兰州 730000;2. 中国电力科学研究院, 北京 100192
基金项目:国家重点基础研究发展计划(973计划)项目(2013CBA01808);国家自然科学基金项目(41275061)资助
摘    要:在检验CMIP3模式比较计划中模式在中国地区的温度模拟效果的基础上,选取模拟效果相对较好的HadCM3、EACHE5模拟结果,采用Kudryavtsev方法,应用数字化土壤和植被资料,借助Arc-GIS,对未来50 a中国地区在A2情景下的冻土空间变化趋势进行了模拟计算. 结果表明,在A2情景下,未来50 a中国地区的冻土呈现出退缩趋势,在2050年,多年冻土在青藏高原地区的巴颜喀拉山-唐古拉山之间、冈底斯山地区出现退化,中国的冻土面积较2006年减少约10.7%.

关 键 词:CMIP3  中国冻土  气候变化  冻土变化  
收稿时间:2013-08-10
修稿时间:2013-11-06

Area change of the frozen ground in China in the next 50 years
WANG Chenghai,JIN Shuanglong,SHI Hongxia. Area change of the frozen ground in China in the next 50 years[J]. Journal of Glaciology and Geocryology, 2014, 36(1): 1-8. DOI: 10.7522/j.issn.1000-0240.2014.0001
Authors:WANG Chenghai  JIN Shuanglong  SHI Hongxia
Affiliation:1. College of Atmospheric Sciences / Key Laboratory of Arid Climatic Change and Disaster Reduction of Gansu Province, Lanzhou University, Lanzhou 730000, China;2. China Electric Power Research Institute, Beijing 100192, China
Abstract:Two models (HadCM3 and EACHE5), which have good ability for temperature simulation in China, are used to calculate the distribution of frozen ground in China, based on testing of the model performance of the Couple Model Intercomparison Project (CMIP3). The trend of frozen ground change in spatial distribution under Scenario A2 in 2006-2050 was calculated by the Kudryavtsev method with ArcGIS and using the datasets of digital soil and vegetation. In the next 50 years, the frozen ground in China will shrink. In 2050, permafrost on the Tibetan Plateau between the Bayan Har Mountains and Tanggula Range and in the Transhimalaya will degenerate. As compared with that in 2006, the frozen ground area in China will decrease about 10.7%.
Keywords:Couple Model Intercomparison Project (CMIP3)  frozen ground in China  climate change  frozen ground change
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