地理研究

地理研究 ›› 1989, Vol. 8 ›› Issue (3): 21-29.doi: 10.11821/yj1989030003

• 论文 • 上一篇    下一篇

论山地气候带和气候型

毛政旦   

  1. 湖南师范大学地理系
  • 收稿日期:1987-09-20 修回日期:1988-05-09 出版日期:1989-09-15 发布日期:1989-09-15

CLIMATE ZONE AND CLIMATE TYPN IN MOUNTAINOUS REGIONS

Mao Zhengdan   

  1. Department of Geography, Hunan Normal University
  • Received:1987-09-20 Revised:1988-05-09 Online:1989-09-15 Published:1989-09-15

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被引次数

45 | 5

摘要： 本文论述了山地高度气候带与纬度气候带在形式上的联系和物理成因上的区别;在达种认识的基础上提出了划分山地高度气候带的基本原则,并提出山地最基本的气候型有四个,即高山气候,谷地气候,坡地气侯和高原气候。

关键词: 山地气候, 气候分类, 气候带, 气候型

Abstract: The formal connections and physical differences between climate zone of the height of mountainous region (CZHMR) and latitude climate are discussed, and on the basis of this acknowledge, the radical principles of dividing CZHMR is presented:(1) The principle of correspondent standard. This means, the standard of dividing CZHMR should be in correspondence with latitude climate zone, so that the two climate zone may be united in one climatic system.(2) The principle of basic zone.This means when we divide the CZHMR, We should determine the latitude climate zone where mountains and plainsare situated,(3) The principle of zonal and azonal,This means we should consider the azonal factors of mountainous region as well as zonal factors,(4) The principle of Iandscape. This means the position of the CZHMR should be in correspondence with the landscape of mountainous region,At the last part of this paper, the division climatic type of mountainous region is discussed, e.g. (a) mountain climate. (b) valley clmmate. (c) slope climate. (d) plateau climate.

Key words: Climate of mountainous region, Climate classification, Climatic zones, Climatic type.