冰川;物质平衡;末端变化;雪冰融水;冰储量;哈密;新疆," /> 冰川;物质平衡;末端变化;雪冰融水;冰储量;哈密;新疆,"/> glacier,material balance,glacier terminal,glaciersnow melt water,glacier storage,Hami region,Xinjiang ,"/> 哈密地区冰川变化趋势分析

干旱区研究 ›› 2014, Vol. 31 ›› Issue (1): 27-31.

• 水土资源 • 上一篇    下一篇

哈密地区冰川变化趋势分析

谢伟1,姜逢清2   

  1. 1. 哈密水文水资源勘测局,新疆 哈密 8390002. 中国科学院新疆生态与地理研究所,新疆乌鲁木齐 830011
  • 收稿日期:2012-11-19 修回日期:2013-05-23 出版日期:2014-01-15 发布日期:2014-02-28
  • 作者简介:谢伟(1979-),男,工程师,主要从事水文水资源勘测和冰川水文的研究工作.E-mail:xiewei6223@126.com
  • 基金资助:

    国家自然科学基金(41171378);哈密榆树沟冰川水资源研究(Y150K11001

Change Trend of Glaciers in the Hami Region

XIE Wei1,JIANG Feng-qing2   

  1. 1. Hami Bureau of Hydrological and Water Resources Survey, Hami 839000, Xinjiang, China;
    2. Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
  • Received:2012-11-19 Revised:2013-05-23 Published:2014-01-15 Online:2014-02-28

摘要: 雪冰融水是哈密地区地表径流的一种主要方式。受全球气候变暖的影响,哈密地区的冰川处于加速融化的阶段,水资源成为哈密地区发展的主要瓶颈。通过对哈密地区冰川物质平衡、面积、厚度、冰川区水文气象等参数的观测,预测冰川水文和水资源的变化,为更好地利用好哈密地区有限的水资源,为可持续发展,提出应对措施。

关键词: font-size: 10.5pt, mso-bidi-font-family: 宋体, mso-font-kerning: 1.0pt, mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, 冰川;物质平衡;末端变化;雪冰融水;mso-bidi-language: AR-SA">冰川;物质平衡;末端变化;雪冰融水;font-size: 10.5pt, mso-bidi-font-family: 宋体, mso-font-kerning: 1.0pt, mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, mso-bidi-language: AR-SA, mso-ascii-font-family: 'Times New Roman', 冰储量mso-bidi-font-size: 12.0pt">冰储量font-size: 10.5pt, mso-bidi-font-family: 宋体, mso-font-kerning: 1.0pt, mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, ;哈密;新疆')">mso-bidi-language: AR-SA">;哈密;新疆

Abstract: Glaciersnow melt water in the main form of surface runoff in the Hami region, Xinjiang, China. Affected by global climate warming, the glaciers in the Hami region are currently at the accelerating melt stage, and the shortage of water resources is the main restriction factor for social and economic development in the Hami region. In this study, the values of material balance, area and thickness of glaciers and the hydrological and meteorological data in the Hami region were measured and observed so as to predict the change trend of glacial hydrology and water resources, provide the references for further utilizing limited water resources, and work out the measures for the local sustainable development. The results revealed that the area and thickness of the glaciers in both Yushugou and Miaoergou valleys were in a slow reduction, a violent change of fluvial recharge will not occur in next decades, and such change trend will continue in the future.

Key words: font-size: 10.5pt, mso-bidi-font-family: 宋体, mso-font-kerning: 1.0pt, mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, glacier')">mso-bidi-language: AR-SA" lang="EN-US">glacier, material balance, glacier terminal, glacierfont-size: 10.5pt, mso-bidi-font-family: MingLiU_HKSCS, mso-font-kerning: 1.0pt, mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, mso-bidi-language: AR-SA, mso-hansi-font-family: MingLiU_HKSCS, mso-ascii-font-family: MingLiU_HKSCS">font-size: 10.5pt, mso-bidi-font-family: 宋体, mso-font-kerning: 1.0pt, mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, snow melt water')">mso-bidi-language: AR-SA" lang="EN-US">snow melt water, glacier storage, Hami region, Xinjiang