globalchange  > 气候变化与战略
CSCD记录号: CSCD:5124271
论文题名:
西藏高原气候变化及其差异性
其他题名: Climate change and its regional differences over the Tibet Plateau
作者: 杨春艳1; 沈渭寿2; 林乃峰2
刊名: 干旱区地理
ISSN: 1000-6060
出版年: 2014
卷: 37, 期:2
语种: 中文
中文关键词: 西藏 ; 日照时数 ; 气温 ; 降水 ; 风速 ; 相对湿度
英文关键词: Tibet Plateau ; sunshine duration ; temperature ; precipitation ; wind speed ; relative humidity
WOS学科分类: METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向: Meteorology & Atmospheric Sciences
中文摘要: 利用西藏高原38个气象站点1961-2010年逐月气象资料,采用气候倾向率、累积距平及 GIS空间插值方法,研究了近50a来西藏及各分区气象要素的时空演变规律,揭示了西藏不同区域气候变化的差异性。结果表明:近50a来,西藏总体呈现出日照略增、温度升高、降水增加、风速减小、平均相对湿度略有上升趋势,年平均日照时数倾向率3.04 h/10 a,年平均气温倾向率0.58 ℃/10a,多年平均降水量倾向率12.5 mm/10a,年平均风速倾向率-0.13 m·s~(-1)·(10a)~(-1)、年平均相对湿度倾向率0.1%/10a。根据地貌分区的各区域气象要素分布及变化程度差异较大,藏北高原区日照时数最长,但呈减少趋势,藏东高山深谷区日照时数最短,增加趋势明显;藏南山原湖盆谷地区年平均气温最高,升温幅度较小,藏北高原区年平均气温最低,升温幅度最大;藏东高山深谷区年平均降水量最多,藏北高原区最少,藏南山原湖盆谷地区降水量增加较明显;藏北高原区平均风速最大,藏东高山深谷区最小,所有区域平均风速均呈先增加后减小趋势;喜马拉雅高山区、藏东高山深谷区相对湿度较大,藏北高原区、藏南山原湖盆谷地区较小,西藏各区平均湿度均有所上升。
英文摘要: On basis of the monthly data for the period 1961-2010 collected from 38 observational stations over the Tibet Plateau,by means of the climate tendency rate,accumulative anomaly and GIS spatial interpolation methods, the temporal-spatial variations of climatic variables over the Tibet in the recent 50 years were systematically studied,and the differences of climate change in different sub-regions were shown. The results indicated that: in the last 50 years, Tibet showed an increase of sunshine (with the linear tendency rate of 3.04 h/10 a), temperature(0.58 °C/ 10 a),precipitation(12.5 mm/10 a),decrease of wind speed(0.13 m ? s~(-1) ? 10 a~(-1)),and slightly rising trend of the average relative humidity (0.1 %/10 a). Distribution and change of the climate facters in different regions divided by geomorphologic situation are remarkable. Sunshine is longest in the northern Tibet Plateau,with a trend of decrease, while shortest in high mountains and deep valleys regions of east Tibet,but increased obviously. Annual mean temperature is highest in Lake Basin Valley Region of south Tibet,with slowly rising rate,and lowest in northern Tibet Plateau,warming fastest. The most average annual precipitation is in northern Tibet Plateau, while least in east Tibet,and precipitation increases obviously in Lake Basin Valley Region of south Tibet. Average wind speed is maximum in northern Tibet Plateau,minimum in high mountains and deep valleys regions of east Tibet, and all regions showed increased first and then decreased trend. Relative humidity is high in Himalaya Mountains region and in high mountains and deep valleys regions of east Tibet,low in northern Tibet Plateau and in Lake Basin Valley Region of south Tibet, and increase in all regions.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/147726
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作者单位: 1.南京信息工程大学遥感学院, 南京, 江苏 210044, 中国
2.环境保护部南京环境科学研究所, 南京, 江苏 210042, 中国

Recommended Citation:
杨春艳,沈渭寿,林乃峰. 西藏高原气候变化及其差异性[J]. 干旱区地理,2014-01-01,37(2)
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