地理学报 ›› 2015, Vol. 70 ›› Issue (9): 1415-1422.doi: 10.11821/dlxb201509005
收稿日期:
2015-06-07
修回日期:
2015-07-18
出版日期:
2015-09-20
发布日期:
2015-09-20
作者简介:
作者简介:杜建括(1984-), 男, 山东聊城人, 讲师, 研究方向为冰川与全球变化。E-mail:
基金资助:
Jiankuo DU1(), Yuanqing HE2, Shuang LI1, Shijin WANG2, Hewen NIU2
Received:
2015-06-07
Revised:
2015-07-18
Published:
2015-09-20
Online:
2015-09-20
Supported by:
摘要:
玉龙雪山发育着对气候变化响应极为敏感的典型海洋型冰川。基于2008-2013年共5个物质平衡年观测数据,对玉龙雪山规模最大的白水1号冰川物质平衡特征进行分析,为评估横断山区气候和冰川变化之间的关系奠定基础。结果表明:2008-2013年白水1号冰川物质平衡最大值仅为-907 mm w.e.,最小值则达到-1872 mm w.e.。2008年冰川平衡线高度为4972 m,2009-2013年白水1号冰川积累区近乎消失。白水1号冰川积累期主要集中于10月至次年5月,6-9月为强消融期,积累量几乎为零,消融量占全年80%,属冬春季积累型冰川。2008-2009、2011-2012和2012-2013年平均物质平衡梯度为1230 mm w.e. (100 m)-1,消融期物质平衡梯度小于年物质平衡梯度,消融期初与消融期末物质平衡梯度小于100 mm w.e.(100 m)-1。
杜建括, 何元庆, 李双, 王世金, 牛贺文. 横断山区典型海洋型冰川物质平衡研究[J]. 地理学报, 2015, 70(9): 1415-1422.
Jiankuo DU, Yuanqing HE, Shuang LI, Shijin WANG, Hewen NIU. Mass balance of a typical monsoonal temperate glacier in Hengduan Mountains Region[J]. Acta Geographica Sinica, 2015, 70(9): 1415-1422.
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