青藏高原与中国气候

Qinghai-Xizang( Tibet) Plateau and the Climate of China

青藏高原的隆起及相伴出现的现代季风与日益加强的过程,深刻地影响和改变着大高原及周围地区的自然面貌,使我国环境东西分异的特征进一步显著,从而形成现代中国自然地理环境分异的格局,即东部季风区、西北干旱区和青藏高寒区,本文即欲从高原动力、热力作用和高原季风等方面探讨青藏高原对我国气候的影响。

The Uplifting Qinghai-Xizang （Tibet） Plateau and the accompanying strengthening monsoon, deeply control the changes landforms of Plateau, thus forming physical geographical environment of China, namely the monsoon region of east china, arid region of Northwest China and paramos region of Qinghai-Xizang （Tibet） Plateau. This paper introduces the process of uplifting of Qinghai-Xizang （Tibet） Plateau, and discusses some important influences of Qinghai-Xizang （Tibet） Plateau uplift on the climate of China in aspects such as dynamic and thermodynamic and up-to-date advances in this field.