首页 | 本学科首页   官方微博 | 高级检索  
     

长白山的气候特征及北坡垂直气候带
引用本文:杨美华. 1981: 长白山的气候特征及北坡垂直气候带. 气象学报, (3): 311-320. DOI: 10.11676/qxxb1981.034
作者姓名:杨美华
作者单位:1.东北师范大学地理系
摘    要:长白山是温带大陆季风型高山气候。北坡有明显的垂直气候带、自下而上为山地针阔混交林气候带、山地针叶林气候带、山地岳桦林气候带、高山灌丛气候带、高山荒漠气候带。

收稿时间:1979-10-08
修稿时间:1980-03-22

THE CLIMATIC FEATURES OF CHANGBAISHAN AND ITS VERTICAL CLIMATIC ZONE ON THE NORTHERN SLOP
Yiang Mei-hua. 1981: THE CLIMATIC FEATURES OF CHANGBAISHAN AND ITS VERTICAL CLIMATIC ZONE ON THE NORTHERN SLOP. Acta Meteorologica Sinica, (3): 311-320. DOI: 10.11676/qxxb1981.034
Authors:Yiang Mei-hua
Affiliation:1.Department of Geography, Jilin Normal University
Abstract:The climate of Changbaishan is Alpine Climate of monsoon types in the temperate zonal continent. Apparently vertical climatic zone on northern slope of Changbaishan, in the order from the lower position to the upper, may be divided into the climatic zone of mountainous mixed forest of needle-leaved and broad leaved; The climatic zone of mountainous needle-leaved forest; the climatic zone of Alpine bush-wood and the climatic zone of Alpine desert.
Keywords:
本文献已被 CNKI 等数据库收录!
点击此处可从《气象学报》浏览原始摘要信息
点击此处可从《气象学报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号