水土保持研究2017，Vol.24Issue(6)：262-266,272,6.
近50年来全球变暖背景下青藏高原气温变化特征
Change of Temperature in The Tibetan Plateau in the Context of Global Warming in Recent 50 Years
吴成启 1唐登勇2
作者信息
- 1. 南京信息工程大学环境科学与工程学院,南京210044
- 2. 河北省石家庄市赞皇县气象局,石家庄050000
- 折叠
摘要
Abstract
We use daily temperature climate statistics of the Tibetan Plateau from 1961 to 2010,and used the linear regression equation,Mann-Kendall mutation testing and other methods to study the spatiotemporal trend of the temperature and climate of the plateau.The results show that:(1) the increase rate of the average annual temperature of the plateau is 0.022 8 ℃C,after 1993,annual average temperature value was high,and average temperatures in the southern region was higher,while the annual average temperature was low in the central region,and abrupt change of temperature in Tibetan Plateau occurred in 1996;(2) the average annual temperature presented the significant seasonal variation,and the average annual temperature trend under four seasons was incremental,warming was the biggest in the spring,and the warming was slight in winter;(3) it was concluded that the average annual presented the distribution characteristics of types of South-Center-North and South-North based on EOF analysis on the average annual temperature.关键词
青藏高原/气温/线性回归/曼—肯德尔/EOFKey words
Tibetan Plateau/temperature/linear regression/Mann-Kendall/EOF分类
天文与地球科学引用本文复制引用
吴成启,唐登勇..近50年来全球变暖背景下青藏高原气温变化特征[J].水土保持研究,2017,24(6):262-266,272,6.
