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	中国干旱区与季风区夏季气温变化特征对比
其他题名	Comparison of summer temperature change characteristics between arid region and monsoon region in China in recent 46 years
	黄斌 1; 王劲松 1; 张洪芬 2
来源期刊	干旱区地理
ISSN	1000-6060
出版年	2010
卷号	33 期号:6 页码:874-878
中文摘要	利用1961-2006年西北干旱区139站和东部季风区378站夏季平均气温资料, 采用趋势系数、相关性检验等方法, 对比分析了两个区域夏季气温的时间和空间变化特征、气温变幅分布, 并对产生变化的原因进行了初步探讨. 结果表明: 受气候变暖大背景的影响, 西北干旱区和东部季风区夏季气温变化均为波动式上升趋势, 但由于地理位置的差异, 受夏季风影响不同, 导致西北干旱区(0.24℃/10 a)的升温趋明显高于季风区(0.11℃/10 a), 同时明显高于相同纬度区域的季风区 (0.15℃/10 a)气温变化趋势. 两个区域气温变幅空间变化分布上都存在明显的升温区域和气温变化相对较弱的区域, 季风区在黄河中下游以南地区到长江中下游以北的广大地区变化不明显, 黄河中下游以北的华北、东北地区有相对较明显的升温趋势; 西北干旱区以明显的升温为主, 尤其是以青海西部至蒙古高原西部形成的一带状区域为主要明显升温区, 其最大升温率达到0.93℃/10 a, 变化相对较弱的区域主要位于吐鲁番盆地和塔里木盆地
英文摘要	Based on the data of 139 stations in arid area of northwest China and 378 stations in eastern monsoon area during 1961 to 2006, and with the help of the methods of the trend coefficient, related test, and comparative analysis of the two areas’ summer mean temperature changes, the temporal and spatial distribution characteristics of temperature change were analyzed, and the change reasons were discussed. The results show that temperature change was resulted in by the background of climate warming, and summer mean temperature was taken the shape of fluctuations with upward trend in two areas. However, because of geographical position ifferences, the summer monsoon’s different effects, the warming trend in northwest arid area (0. 24 ℃/10 a) was significantly much higher than that in eastern monsoon area(0. 11 ℃/10a), and at the same time significantly higher than that in the same latitude’s monsoon area (0.15 ℃/10 a). According to the spatial distribution of summer mean temperature amplitude, there are obviously rising temperature region and weakly rising temperature region in both of two areas. In the monsoon area, the temperature change is not obvious in the vast area which stretches from the south of the middle and lower reaches of the Yellow River to the north of the middle and lower reaches of the Yangtze River, meanwhile, the rising temperature trend is relatively clear in the north China and northeast China which are in the north of the middle and lower reaches of the Yellow River. The arid area in northwest China is characterized by the distinctly rising temperature, especially in the area which is from the west part of Qinghai to the west part of the Mongolia Plateau with maximum temperature rising rate of 0.93 ℃/10 a, meantime, there is a area mainly located in the Turpan Basin and Tarim Basin with relatively weak rising temperature
中文关键词	西北干旱区 ; 东部季风区 ; 气温变化 ; 夏季
英文关键词	arid region of northwest China eastern monsoon region temperature change summer
语种	中文
国家	中国
收录类别	CSCD
WOS类目	METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向	Meteorology & Atmospheric Sciences
CSCD记录号	CSCD:4103237
来源机构	中国气象局兰州干旱气象研究所
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/225029
作者单位	1.中国气象局兰州干旱气象研究所, 甘肃省干旱气候变化与减灾重点实验室;;中国气象局干旱气候变化与减灾重点开放实验室, 兰州, 甘肃 730020, 中国; 2.甘肃省庆阳市气象局, 庆阳, 甘肃 745000, 中国
推荐引用方式 GB/T 7714	黄斌,王劲松,张洪芬. 中国干旱区与季风区夏季气温变化特征对比[J]. 中国气象局兰州干旱气象研究所,2010,33(6):874-878.
APA	黄斌,王劲松,&张洪芬.(2010).中国干旱区与季风区夏季气温变化特征对比.干旱区地理,33(6),874-878.
MLA	黄斌,et al."中国干旱区与季风区夏季气温变化特征对比".干旱区地理 33.6(2010):874-878.