摘要
青藏高原的热环境的变化,不仅对我国,对亚洲乃至北半球的大气环流均具有极为重要的作用,直接影响着东亚季风气候的形成和演变。用亚东-格尔木-锡铁山走廊域的地学剖面实测温度数据和青藏高原MODIS遥感影像数据,研究分析了该走廊域的热环境特征。研究表明,在研究区域内热环境分布具有明显的南北条带性:西北部的温度偏低,东南部次之,中东部温度最高。
The changes of thermal environment in Qinghai-Tibet Plateau are very important not only for China, but also Asia and the northern hemisphere atmospheric circulation, which have a direct impact on the formation and evolution of the East Asia monsoon climate. In the paper the thermal environment characteristic of Yadong-Golmud-Xitie Mountain corridor was studied and analysed. The results of study show that the distribution of the thermal environment has obvious north and south strip in the studied area: the northwestern temperature is somewhat low, the southeast is next, and the middle eastern is highest.
出处
《安徽理工大学学报(自然科学版)》
CAS
2008年第3期1-4,共4页
Journal of Anhui University of Science and Technology:Natural Science
关键词
热红外遥感
亚东-格尔木-锡铁山
热环境
区划
thermal infrared remote sensing
Yadong-Golmud-Xitie Mountain
thermal environment
partion