贾旭;文汉江;刘焕玲;董杰;陈柏含;

• 1:辽宁工程技术大学测绘与地理科学学院
• 2:中国测绘科学研究院
• 3:城市空间信息工程北京市重点实验室

摘要(Abstract)：

针对地表沉降与地下水储量变化相关性这一问题。该文选取华北地区这一地表沉降典型区域,①利用2003—2009年GRACE月重力场模型和全球陆地数据同化系统GLDAS-Noah模型求得华北地区地下水储量平均变化速率为-16±2 mm/a;②利用1999-2009年275个GPS站点垂直方向速度求得华北地区地表沉降平均速率为-30 mm/a;③结合2003—2009年中国地面2 472台站降水资料和WGHM全球水文模型进行分析。结果表明,华北地区地下水储量变化与年降水量的关系并不明显,地面沉降与降水量的相关性也不明显,但与地下水储量有着显著的关联,地表沉降严重地区的地下水储量下降趋势较大,华北地区地下水储量变化与地表沉降变化整体呈现下降趋势。

关键词(KeyWords)： GRACE;GPS速度场;地表沉降;地下水储量

Abstract:

Keywords:

基金项目(Foundation): 民用航天预先研究项目;; 高分辨率对地观测系统重大专项;; 中国测绘科学研究院基本科研业务费资助项目(7771811);; 辽宁省教育厅辽宁省高等学校基本科研项目(LJ2017QL008);; German Academic Exchange Service(DAAD)Thematic Network Program “Modern Geodetic Space Techniques for Global Change Monitoring”(57421148);; 武汉大学地球空间环境与大地测量教育部重点实验室开放基金资助项目(18-01-05);; 城市空间信息工程北京市重点实验室经费资助项目(2019211)

作者(Author): 贾旭;文汉江;刘焕玲;董杰;陈柏含;

Email:

DOI: 10.16251/j.cnki.1009-2307.2020.03.003

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