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基于Sentinel-1A SAR数据的呼和浩特城区地表形变分析

尹承深, 刘全明, 王福强. 基于Sentinel-1A SAR数据的呼和浩特城区地表形变分析[J]. 中国地质灾害与防治学报, 2023, 34(2): 73-81. doi: 10.16031/j.cnki.issn.1003-8035.202112023
引用本文: 尹承深, 刘全明, 王福强. 基于Sentinel-1A SAR数据的呼和浩特城区地表形变分析[J]. 中国地质灾害与防治学报, 2023, 34(2): 73-81. doi: 10.16031/j.cnki.issn.1003-8035.202112023
YIN Chengshen, LIU Quanming, WANG Fuqiang. Surface deformation analysis of Hohhot urban area based on SAR data from Sentinel-1A[J]. The Chinese Journal of Geological Hazard and Control, 2023, 34(2): 73-81. doi: 10.16031/j.cnki.issn.1003-8035.202112023
Citation: YIN Chengshen, LIU Quanming, WANG Fuqiang. Surface deformation analysis of Hohhot urban area based on SAR data from Sentinel-1A[J]. The Chinese Journal of Geological Hazard and Control, 2023, 34(2): 73-81. doi: 10.16031/j.cnki.issn.1003-8035.202112023

基于Sentinel-1A SAR数据的呼和浩特城区地表形变分析

  • 基金项目: 国家自然科学基金项目(52069020)
详细信息
    作者简介: 尹承深(1996-),男,山东聊城人,硕士研究生,主要从事遥感水利与信息化技术研究。E-mail:cheng20192020@emails.imau.edu.cn
    通讯作者: 刘全明(1973-),男,内蒙古四子王旗人,博士研究生,副教授,主要从事测绘工程教育与定量遥感反演理论及应用研究。E-mail:nndlqm@sina.com
  • 中图分类号: P642

Surface deformation analysis of Hohhot urban area based on SAR data from Sentinel-1A

More Information
  • 为了实现对呼和浩特市城区形变监测,采用永久散射体合成孔径雷达干涉测量(PS-InSAR)技术,对2017年3月—2021年4月期间25景呼和浩特市城区Sentinel-1A数据进行时序干涉处理,提取了城区地表沉降信息,并分析了主要沉降中心沉降原因。结果表明:呼和浩特市城区地表存在5个明显的沉降中心,整体地表平均年沉降速率3.65 mm/a,平均累计沉降量为15.50 mm,其沉降主要原因是由于地下水过度开采。Sentinel-1A数据具有时间基线短、影像数量足、数据免费等优点,利于InSAR时序分析,可满足同类城区地表形变监测工作,服务城市安全。

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  • 图 1  研究区遥感影像图

    Figure 1. 

    图 2  PS-InSAR时空基线图

    Figure 2. 

    图 5  A区平均形变速率特征图

    Figure 5. 

    图 3  呼和浩特市2017—2021年地表累计形变量

    Figure 3. 

    图 4  2017—2021年研究区平均形变速率图

    Figure 4. 

    图 6  实地调查照片

    Figure 6. 

    表 1  研究所采用的Sentinel-1A数据参数

    Table 1.  Summary of the Sentinel-1A data parameters used in the study

    影像编号成像日期空间基线距/m时间基线距/d影像编号成像日期空间基线距/m时间基线距/d
    12017-03-19 −34.87−564142019-04-02−28.33180
    22017-04-12−37.39−540152019-06-01−23.04240
    32017-06-1126.72−480162019-08-12−78.11312
    42017-07-29−40.10−432172019-10-1153.56372
    52017-10-09−33.23−360182019-12-1087.43432
    62017-12-0845.08−300192020-02-0862.98492
    72018-02-06−31.88−240202020-04-0863.07552
    82018-04-0712.50−180212020-05-14−30.41588
    92018-06-06−22.68−120222020-08-0629.23672
    102018-08-05−18.48−60232020-10-05−33.29732
    112018-10-040.000242020-12-0423.03792
    122018-12-0348.1060252021-04-035.72912
    132019-02-0145.28120
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出版历程
收稿日期:  2021-12-20
修回日期:  2022-10-10
录用日期:  2022-10-12
刊出日期:  2023-04-25

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