杨美华. 1981. 长白山的气候特征及北坡垂直气候带[J]. 气象学报, 39(3):311-320, doi:10.11676/qxxb1981.034
长白山的气候特征及北坡垂直气候带
THE CLIMATIC FEATURES OF CHANGBAISHAN AND ITS VERTICAL CLIMATIC ZONE ON THE NORTHERN SLOP
投稿时间:1979-10-08  修订日期:1980-03-22
DOI:10.11676/qxxb1981.034
中文关键词:  
英文关键词:
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作者单位
杨美华 东北师范大学地理系 
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中文摘要:
      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。
英文摘要:
      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.
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