摘要
首先利用EOF方法,分析了0°~180°E,0°~60°N范围内100,150,200,250,300,400,500hPa等层次上温度场的时空变化特征,结果表明,青藏、伊朗高原的热力异常在300hPa温度场上有明显的体现。然后利用SVD方法,分析了青藏、伊朗高原地区300hPa温度场异常与我国区域气温的关系,分析表明:(1)伊朗高原大部和青藏高原中部、西北部6~8月300hPa温度与我国长江流域和江淮之间同期的气温有显著的正相关关系;(2)青藏高原东部、西北部4~5月300hPa温度与我国长江流域偏南地区6~8月的气温有显著的正相关关系。
Firstly, thetemporal and spatial variations of temperature fields of 100, 150, 200, 250, 300, 400 and 500 hPain 0°~180°E, 0°~60°N were analyzed by using EOF method. Resultsshow that 300 hPa temperature field can reflect the thermodynamic anomaly of Iranian and Qinghai-Xizang Plateaus. Secondly, the relationbetween 300 hPa temperature and regional air temperature of China is analyzed by using SVD expansion. Results show:(1) There is a positive correlation between 300 hPatemperature in the most of Iranian Plateau, thecenter and north-west of Qinghai-Xizang Plateau and air temperature in Changjiang River and Huaihe valley in June~August. (2) 300 hPa temperature in the east, northwestof Qinghai-Xizang Plateau in April~May positively correlates to air temperature in the southern-toward area in Changjiang River valley in June~August.
出处
《高原气象》
CSCD
北大核心
2004年第3期323-329,共7页
Plateau Meteorology
基金
中国科学技术大学青年基金项目"青藏
伊朗高原地区热力异常与我国区域气候异常的关系"资助
关键词
青藏高原
伊朗高原
300hPa温度
我国区域气温
Iranian Plateau
Qinghai-Xizang Plateau
300 hPa temperature
China air temperature