冰川冻土 ›› 2020, Vol. 42 ›› Issue (2): 318-331.doi: 10.7522/j.issn.1000-0240.2019.0035
车彦军1,2(), 张明军1(
), 李忠勤1,3, 金爽3, 王文彬3, 王圣杰1
收稿日期:
2018-06-11
修回日期:
2019-03-16
出版日期:
2020-08-31
发布日期:
2019-03-16
通讯作者:
张明军
E-mail:che_yanjun@126.com;mjzhang2004@163.com
作者简介:
车彦军(1988 - ), 男, 甘肃武山人, 2017年在西北师范大学获得博士学位, 从事全球变化与水循环过程、 冰川与气候作用机理研究. E-mail:che_yanjun@126.com
基金资助:
Yanjun CHE1,2(), Mingjun ZHANG1(
), Zhongqin LI1,3, Shuang JIN3, Wenbin WANG3, Shengjie WANG1
Received:
2018-06-11
Revised:
2019-03-16
Online:
2020-08-31
Published:
2019-03-16
Contact:
Mingjun ZHANG
E-mail:che_yanjun@126.com;mjzhang2004@163.com
摘要:
物质平衡是冰川与气候相互作用的关键桥梁, 对气候变化非常敏感。基于青冰滩72号冰川2008 - 2014年冰面花杆和雪坑的观测资料, 结合Landsat系列卫星影像, 利用零平衡线法对青冰滩72号冰川的物质平衡进行计算和分析。结果表明: 青冰滩72号冰川2008 - 2014年平均物质平衡梯度为(0.86 ± 0.19) m w.e.?(100m)-1; 平衡线高度在(4 109 ± 23) ~ (4 317 ± 92) m a.s.l.之间变化, 平均为(4 167.5 ± 33.2) m a.s.l。同时, 青冰滩72号冰川年净物质平衡介于-1.23 m w.e. ~ +0.31 m w.e., 年平均为-0.38 m w.e., 累积物质平衡为-2.27 m w.e.。此外, 与位于天山地区图尤克苏冰川、 乌鲁木齐河源1号冰川平衡线高度和累积物质平衡的比较发现, 青冰滩72号冰川平衡线高度和物质平衡的变化与图尤克苏冰川相似, 而与乌鲁木齐河源1号冰川的差异相对较大。
中图分类号:
车彦军, 张明军, 李忠勤, 金爽, 王文彬, 王圣杰. 2008 - 2014年青冰滩72号冰川物质平衡特征分析[J]. 冰川冻土, 2020, 42(2): 318-331.
Yanjun CHE, Mingjun ZHANG, Zhongqin LI, Shuang JIN, Wenbin WANG, Shengjie WANG. Understanding the mass balance characteristics of Qingbingtan Glacier No. 72 during the period of 2008 - 2014[J]. Journal of Glaciology and Geocryology, 2020, 42(2): 318-331.
表1
2008 - 2014年8 - 10月Landsat系列影像(P147R31)质量评估信息"
序号 | 年份 | 文件名 | 对应日期 | 影像评估 |
---|---|---|---|---|
1 | 2009 | LT51470312009273IKR01 | 2009-09-30 | 清晰 |
2 | 2010 | LT51470312010228IKR01 | 2010-08-16 | 清晰 |
3 | 2011 | LT51470312011215KHC01 | 2011-08-03 | 清晰 |
4 | 2011 | LT51470312011231KHC01 | 2011-08-19 | 清晰 |
5 | 2012 | LE71470312012242PFS00 | 2012-08-29 | 清晰 |
6 | 2013 | LE71470312013276SG100 | 2013-10-03 | 清晰 |
7 | 2013 | LC81470312013252LGN00 | 2013-09-09 | 有积雪 |
8 | 2014 | LE71470312014263PFS00 | 2014-09-20 | 少量积雪 |
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