摘要
中国东部 (青藏高原以东 )冬季形成低温的“冷槽” ,而夏季形成高温的“热脊” .冷槽、热脊形成的机制是不同时空尺度的环流和青藏高原的动力和热力作用 .冷槽。
Owing to the influence of the atmospheric circulation with the different time and space, and the function of the dynamic and heat of the Qinghai Xizang Plateau, it is formed the “cold trough”(low temperature trough) in winter and “Thermal backbone”(high temperature backbone) in the east of China. It is a very complex problem that the formation of the “cold trough” and “thermal backbone” is influenced by many factors. Among them, the dynamic and heat of the Qinghai Xizang Plateau are important factors. The formations of the “cold trough” and “thermal backbone” can influence the climate in east of China.
出处
《安徽师范大学学报（自然科学版）》
CAS
2001年第2期141-143,共3页
Journal of Anhui Normal University(Natural Science)
