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題名 應用PS-InSAR於大屯火山地表形變之長期監測
A Long-term Surface Deformation Monitoring over Datun Volcano Group Using PS-InSAR Technique
作者 洪翊甯
Hung, Yi Ning
貢獻者 林士淵
Lin, Shih Yuan
洪翊甯
Hung, Yi Ning
關鍵詞 大屯火山群
地表形變
PS-InSAR
日期 2012
上傳時間 1-十月-2013 11:51:28 (UTC+8)
摘要 大屯火山群為台灣地區最大之火山群，為了解此火山群之運動情況，已有許多研究單位於此區進行許多內部岩漿庫與外部地表之監測，由近年研究發現，大屯火山群仍含有活動之岩漿庫，為一休眠之活火山，由於大屯火山之地理位置接近台北盆地，若火山噴發即會造成嚴重之傷害，故對於大屯火山之監測，為刻不容緩之課題。遙感探測（Remote Sensing）技術為偵測地表形變常用之方法，其中的合成孔徑雷達干涉（InSAR）與合成孔徑雷達差分干涉（D-InSAR）技術具有大範圍獲取地表形變資訊，並可達公分等級精度之優點，但由於植被和山區之同調性較低，難以獲取形變資訊，為突破此限制，學者提出以永久散射體合成孔徑雷達差分干涉（PS-InSAR）技術偵測地表形變。本研究之目的為獲取長時間序列大屯火山外部地表形變資訊，而由於研究區域位於山區且植被覆蓋茂盛，影響InSAR與D-InSAR技術之偵測成果，故本研究實施PS-InSAR技術偵測單點之地表形變量，並使用ERS-2、ASAR、PALSAR三種衛星影像，組成1995年至2011年之長時間序列，得到時間序列內永久散射點之地表形變平均速度場（Velocity Field），發現大屯火山群上之地表形變，在同一地區並非持續的抬升或沉降，而存有隨時間、空間之不同，地表形變不規則之情況，本研究將此成果與GPS與精密水準資料檢核，得到趨勢符合真實地表形變情形之成果，證實以PS-InSAR技術偵測大屯火山群之能力。
Although there was no eruption occurring for three hundred thousand years, the existing ground monitoring reveals that Datun volcanoes may be still active. As Datun volcano group is very close to Taipei City, serious damages would occur if the volcanoes erupted. Therefore it is critical to understand the behaviors of the volcanoes. To this end, we used space-borne Synthetic Aperture Radar (SAR) data and interferometric processing techniques to detect sub-centimeter level ground deformation. Moreover, in order to achieve a long term monitoring, multiple radar data, including ERS-2, ASAR and PALSAR covering from 1995 to 2011, were employed. Through the Persistent Scatterers Interferometric SAR (PS-InSAR) processing, the ground displacement rate occurring over Datun volcanoes was derived. We notice that ground displacement over Datun volcano group is inconsistence with time. The results were verified with ground leveling data and GPS observations and were proved reliable.
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描述 碩士
國立政治大學
地政研究所
100257026
101
資料來源 http://thesis.lib.nccu.edu.tw/record/#G0100257026
資料類型 thesis
dc.contributor.advisor 林士淵zh_TW
dc.contributor.advisor Lin, Shih Yuanen_US
dc.contributor.author (作者) 洪翊甯zh_TW
dc.contributor.author (作者) Hung, Yi Ningen_US
dc.creator (作者) 洪翊甯zh_TW
dc.creator (作者) Hung, Yi Ningen_US
dc.date (日期) 2012en_US
dc.date.accessioned 1-十月-2013 11:51:28 (UTC+8)-
dc.date.available 1-十月-2013 11:51:28 (UTC+8)-
dc.date.issued (上傳時間) 1-十月-2013 11:51:28 (UTC+8)-
dc.identifier (其他 識別碼) G0100257026en_US
dc.identifier.uri (URI) http://nccur.lib.nccu.edu.tw/handle/140.119/61171-
dc.description (描述) 碩士zh_TW
dc.description (描述) 國立政治大學zh_TW
dc.description (描述) 地政研究所zh_TW
dc.description (描述) 100257026zh_TW
dc.description (描述) 101zh_TW
dc.description.abstract (摘要) 大屯火山群為台灣地區最大之火山群，為了解此火山群之運動情況，已有許多研究單位於此區進行許多內部岩漿庫與外部地表之監測，由近年研究發現，大屯火山群仍含有活動之岩漿庫，為一休眠之活火山，由於大屯火山之地理位置接近台北盆地，若火山噴發即會造成嚴重之傷害，故對於大屯火山之監測，為刻不容緩之課題。遙感探測（Remote Sensing）技術為偵測地表形變常用之方法，其中的合成孔徑雷達干涉（InSAR）與合成孔徑雷達差分干涉（D-InSAR）技術具有大範圍獲取地表形變資訊，並可達公分等級精度之優點，但由於植被和山區之同調性較低，難以獲取形變資訊，為突破此限制，學者提出以永久散射體合成孔徑雷達差分干涉（PS-InSAR）技術偵測地表形變。本研究之目的為獲取長時間序列大屯火山外部地表形變資訊，而由於研究區域位於山區且植被覆蓋茂盛，影響InSAR與D-InSAR技術之偵測成果，故本研究實施PS-InSAR技術偵測單點之地表形變量，並使用ERS-2、ASAR、PALSAR三種衛星影像，組成1995年至2011年之長時間序列，得到時間序列內永久散射點之地表形變平均速度場（Velocity Field），發現大屯火山群上之地表形變，在同一地區並非持續的抬升或沉降，而存有隨時間、空間之不同，地表形變不規則之情況，本研究將此成果與GPS與精密水準資料檢核，得到趨勢符合真實地表形變情形之成果，證實以PS-InSAR技術偵測大屯火山群之能力。zh_TW
dc.description.abstract (摘要) Although there was no eruption occurring for three hundred thousand years, the existing ground monitoring reveals that Datun volcanoes may be still active. As Datun volcano group is very close to Taipei City, serious damages would occur if the volcanoes erupted. Therefore it is critical to understand the behaviors of the volcanoes. To this end, we used space-borne Synthetic Aperture Radar (SAR) data and interferometric processing techniques to detect sub-centimeter level ground deformation. Moreover, in order to achieve a long term monitoring, multiple radar data, including ERS-2, ASAR and PALSAR covering from 1995 to 2011, were employed. Through the Persistent Scatterers Interferometric SAR (PS-InSAR) processing, the ground displacement rate occurring over Datun volcanoes was derived. We notice that ground displacement over Datun volcano group is inconsistence with time. The results were verified with ground leveling data and GPS observations and were proved reliable.en_US
dc.description.tableofcontents 目錄
摘要 I
圖目錄 IV
表目錄 VII
第一章 緒論 1
第一節 研究背景與動機 1
第二節 研究目的 4
第三節 文章架構 5
第二章 理論基礎與文獻回顧 7
第一節 合成孔徑雷達影像 7
第二節 雷達干涉原理 12
第三節 長時間序列之雷達干涉處理 20
第四節 小結 29
第三章 研究方法 31
第一節 研究工具 33
第二節 PS-INSAR處理流程 35
第四章 研究成果與檢核 41
第一節 資料選取 41
第二節 研究成果 44
第三節 PS-INSAR成果檢核 44
第五章 成果討論 44
第一節 檢核成果討論 44
第二節 技術執行 44
第六章 結論與建議 44
參考文獻 44		zh_TW
dc.format.extent 9287724 bytes-
dc.format.mimetype application/pdf-
dc.language.iso en_US-
dc.source.uri (資料來源) http://thesis.lib.nccu.edu.tw/record/#G0100257026en_US
dc.subject (關鍵詞) 大屯火山群zh_TW
dc.subject (關鍵詞) 地表形變zh_TW
dc.subject (關鍵詞) PS-InSARzh_TW
dc.title (題名) 應用PS-InSAR於大屯火山地表形變之長期監測zh_TW
dc.title (題名) A Long-term Surface Deformation Monitoring over Datun Volcano Group Using PS-InSAR Techniqueen_US
dc.type (資料類型) thesisen
dc.relation.reference (參考文獻) 中文參考文獻
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