地理学报 ›› 2011, Vol. 66 ›› Issue (9): 1191-1199.doi: 10.11821/xb201109004
黄小燕, 张明军, 王圣杰, 李亚举, 潘淑坤
收稿日期:
2011-04-15
修回日期:
2011-07-05
出版日期:
2011-09-20
发布日期:
2011-09-20
通讯作者:
张明军(1975-), 男, 教授, 博导, 中国地理学会会员(S110007775M), 主要从事气候变化与冰川研究。E-mail: mjzhang2004@163.com
作者简介:
黄小燕(1984-), 女, 湖北宜城人, 硕士研究生, 主要从事全球环境变化方面的研究工作。E-mail: xyhuang0529@sina.cn
基金资助:
教育部新世纪优秀人才支持计划项目(NCET-10-0019); 国家自然科学基金项目(41161012); 陇原青年创新人才扶持计划; 西北师范大学知识与科技创新工程创新团队项目(NWNU-KJCXGC-03-66)
HUANG Xiaoyan, ZHANG Mingjun, WANG Shengjie, LI Yaju, PAN Shukun
Received:
2011-04-15
Revised:
2011-07-05
Online:
2011-09-20
Published:
2011-09-20
Supported by:
The Program for New Century Excellent Talents in Universities by the Education Ministry of China, No. NCET-10-0019; National Natural Science Foundation of China, No.41161012; The Foundation for Young Innovative Scientists in Gansu Province; The Knowledge and Technological Innovation Project of Northwest Normal University, No.NWNU-KJCXGC-03-66
摘要: 采用1960-2009 年112 个地面观测站和21 个探空站气象资料,分析中国西北地区近50 年夏季0 ℃层高度和平均气温变化趋势。结果表明:西北地区近50 年来夏季0 ℃层高度平均值为4675.7 m,在1987 年以前表现为下降趋势,平均每年下降5.6 m,而1987 年以后表现为显著的上升趋势,平均每年上升2.6 m;夏季平均气温与0 ℃层高度变化趋势大致相同,西北气候显著转型前后表现出相反的变化趋势,且1987 年以来夏季平均气温增加急剧,平均每10 年上升0.53 ℃。1960 年以来夏季0 ℃层高度在北京时间08 时该区大部分地区表现出显著的上升趋势,而在20时大部分地区表现出相反的变化趋势,1987 年以来在08 时和20 时大部分地区夏季0 ℃层高度都为上升趋势;50 年来大部分地区夏季平均气温都表现为上升趋势,乌鲁木齐和秦巴山地则表现为显著的下降趋势。西北不同气候区的夏季0 ℃层高度和平均气温变化也有一定的差异。西北地区夏季0 ℃层高度和平均气温具有较好相关性,东部季风区相关性最差,青藏高寒区最好。
黄小燕, 张明军, 王圣杰, 李亚举, 潘淑坤. 中国西北地区近50年夏季0 ℃层高度及气温时空变化特征[J]. 地理学报, 2011, 66(9): 1191-1199.
HUANG Xiaoyan, ZHANG Mingjun, WANG Shengjie, LI Yaju, PAN Shukun. Variation of 0 ℃ Isotherm Height and Ground Temperature in Summer in Northwest China during the Past 50 Years[J]. Acta Geographica Sinica, 2011, 66(9): 1191-1199.
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