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題名 利用SLR及GPS觀測資料估計地心運動之研究
The study of using SLR and GPS observation data to estimate geocenter motion作者 曾義傑
Cheng, Yih-Jack貢獻者 甯方璽
Ning, Fang-Shii
曾義傑
Cheng, Yih-Jack關鍵詞 地心運動
全球定位系統
衛星雷射測距
Geocenter motion
Global positioning system (GPS)
Satellite laser ranging (SLR)日期 2018 上傳時間 27-Aug-2018 14:56:53 (UTC+8) 摘要 地心運動是地球質量的重新分佈和變形，而導致的固態地球形狀中心 (Center of Figure, CF)與地球質量中心(Center of Mass of the Earth System, CM)之間的偏移量。隨著空間大地測量之精度的提高和應用的要求，地心運動研究和估計之重要性與日俱增，因為它是以地球質量中心為原點的各式坐標系統的關鍵。目前地心運動皆以單一觀測技術(如SLR (Satellite Laser Ranging)或GPS(Global Positioning System))進行一階變形法或網形偏移法求解，本研究將結合SLR及GPS觀測資料，以網形偏移法進行研究，評估結合不同觀測方法數據是否可提升地心運動之求解精度。本研究使用2007年至2016年間國際GNSS服務（International GNSS Service, IGS）之GPS觀測資料及部分測站之SLR追蹤GRACE-A（Gravity Recovery and Climate Experiment-A）衛星觀測資料，以GAMIT/GLOBK和Bernese軟體進行地球表面觀測站坐標計算，再應用Helmert坐標轉換求取地心運動量，並利用含有線性項和球諧項之函數進行資料擬合，最後探討地心運動模型之精度。由研究成果顯示2007年至2016年間地心運動於X，Y和Z分量之振幅分別為2.6mm±0.2mm，4.1mm±0.2mm和5.6mm±0.3mm。其年相位於X，Y和Z分量分別為72°，330°和145°，與目前僅用一種觀測技術求解之精度比較有顯著性之提升。
Geocenter motion describes the difference of Center of Figure (CF) respect to Center of Mass of the Earth system (CM) due to the mass re-distribution and deformation of the Earth system. This is a factor that cannot be ignored in the maintenance of the high-precision terrestrial reference frame. As precision requirements and application demands in space geodesy increase, research on estimation of the geocenter motion become increasingly important as the key point to realize a reference frame with its origin fixed to center of mass of the Earth system.In this study, GPS (Global Positioning System) observation data from IGS (International GNSS Service) and SLR (Satellite Laser Ranging) tracking data in the period of 2007 to 2016 are applied to estimate the coordinates of IGS sites on Earth’s surface by using the GAMIT/GLOBK and Bernese software. Then, the Helmert transformation model is used to acquire seven parameters between the ITRF (International Terrestrial Reference Frame) reference frame and the CM reference frame. There are three parameters of them are related to the shift in three axes, which are the results of the geocenter motion. Afterwards, the geocenter motion time series are applied with linear fitting method in order to obtain the amplitudes and phases along three axes of geocenter motion.The annual amplitude of X-, Y-, and Z-components between the years 2007 and 2016 are 2.6±0.2mm, 4.1±0.2mm, and 5.6±0.3mm respectively. The annual phase of X-, Y-, and Z-components are 72°, 330°, and 145° respectively. The accuracy of this study is significant improvement comparing to just using GPS or SLR technique only.參考文獻 一、中文參考文獻周旭華、高布錫，2000，「地心的變化及其原因」，『地球物理學報』，43(2)：160-165。謝蘇銳、李斐、鄢建國，2014，「基於空間大地測量與地球物理方法的地心運動研究與監測進展」，『地球物理學進展』，29(1)：15-24。朱文耀、宋淑麗，2010，「國際地球參考框架 (ITRF) 的原點和無整體旋轉」，『天文學進展』，28(4)：321-332。趙德軍、李潭欣、李婧、陳永祥，2015，「DORIS, GPS 和 SLR 空間大地測量技術匯出的地心運動規律」，『測繪工程』，2015(12):21-24。魏娜、施闖、劉經南，2011，「利用GPS資料反演地心運動」，『武漢大學學報資訊科學版』，36(4)：441-445。陳盈樺，2009，「利用測高衛星、重力衛星、NCEP氣候模型估計地心與 C20 變動」，成功大學測量及空間資訊學系碩士論文：台南。二、外文參考文獻Altamimi, Z., Collilieux, X., & Métivier, L., 2011, “ITRF2008: an improved solution of the international terrestrial reference frame”, Journal of Geodesy, 85(8): 457-473.Altamimi, Z., Collilieux, X., Legrand, J., Garayt, B., and Boucher, C., 2007, “ITRF2005: A new release of the International Terrestrial Reference Frame based on time series of station positions and Earth Orientation Parameters”, Journal of Geophysical Research: Solid Earth, 112(B9).Altamimi, Z., Sillard, P., & Boucher, C., 2002, “ITRF2000: A new release of the International Terrestrial Reference Frame for earth science applications”, Journal of Geophysical Research: Solid Earth, 107(B10).Altamimi, Z., Rebischung, P., Métivier, L., & Collilieux, X., 2016, “ITRF2014: A new release of the International Terrestrial Reference Frame modeling nonlinear station motions”, Journal of Geophysical Research: Solid Earth, 121(8): 6109-6131.Argus, D. 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Retrieved October 22, 2017 from Sedris standards on the World Wide Web: http://standards.sedris.org/18026/text/ISOIEC_18026E_RD_ORM.HTM四、參考書林惠玲、陳正倉. (2011).『應用統計學』四版修訂版，臺北：雙葉書廊有限公司。Hofmann-Wellenhof, B., Lichtenegger, H., & Wasle, E. (2007). GNSS–global navigation satellite systems: GPS, GLONASS, Galileo, and more. Springer Science & Business Media.Seeber, G. (2003). Satellite geodesy: foundations, methods, and applications. Walter de gruyter.Van Sickle, J. (2008). GPS for land surveyors. CRC Press. 描述 碩士
國立政治大學
地政學系
105257033資料來源 http://thesis.lib.nccu.edu.tw/record/#G0105257033 資料類型 thesis dc.contributor.advisor 甯方璽 zh_TW dc.contributor.advisor Ning, Fang-Shii en_US dc.contributor.author (Authors) 曾義傑 zh_TW dc.contributor.author (Authors) Cheng, Yih-Jack en_US dc.creator (作者) 曾義傑 zh_TW dc.creator (作者) Cheng, Yih-Jack en_US dc.date (日期) 2018 en_US dc.date.accessioned 27-Aug-2018 14:56:53 (UTC+8) - dc.date.available 27-Aug-2018 14:56:53 (UTC+8) - dc.date.issued (上傳時間) 27-Aug-2018 14:56:53 (UTC+8) - dc.identifier (Other Identifiers) G0105257033 en_US dc.identifier.uri (URI) http://nccur.lib.nccu.edu.tw/handle/140.119/119594 - dc.description (描述) 碩士 zh_TW dc.description (描述) 國立政治大學 zh_TW dc.description (描述) 地政學系 zh_TW dc.description (描述) 105257033 zh_TW dc.description.abstract (摘要) 地心運動是地球質量的重新分佈和變形，而導致的固態地球形狀中心 (Center of Figure, CF)與地球質量中心(Center of Mass of the Earth System, CM)之間的偏移量。隨著空間大地測量之精度的提高和應用的要求，地心運動研究和估計之重要性與日俱增，因為它是以地球質量中心為原點的各式坐標系統的關鍵。目前地心運動皆以單一觀測技術(如SLR (Satellite Laser Ranging)或GPS(Global Positioning System))進行一階變形法或網形偏移法求解，本研究將結合SLR及GPS觀測資料，以網形偏移法進行研究，評估結合不同觀測方法數據是否可提升地心運動之求解精度。本研究使用2007年至2016年間國際GNSS服務（International GNSS Service, IGS）之GPS觀測資料及部分測站之SLR追蹤GRACE-A（Gravity Recovery and Climate Experiment-A）衛星觀測資料，以GAMIT/GLOBK和Bernese軟體進行地球表面觀測站坐標計算，再應用Helmert坐標轉換求取地心運動量，並利用含有線性項和球諧項之函數進行資料擬合，最後探討地心運動模型之精度。由研究成果顯示2007年至2016年間地心運動於X，Y和Z分量之振幅分別為2.6mm±0.2mm，4.1mm±0.2mm和5.6mm±0.3mm。其年相位於X，Y和Z分量分別為72°，330°和145°，與目前僅用一種觀測技術求解之精度比較有顯著性之提升。 zh_TW dc.description.abstract (摘要) Geocenter motion describes the difference of Center of Figure (CF) respect to Center of Mass of the Earth system (CM) due to the mass re-distribution and deformation of the Earth system. This is a factor that cannot be ignored in the maintenance of the high-precision terrestrial reference frame. As precision requirements and application demands in space geodesy increase, research on estimation of the geocenter motion become increasingly important as the key point to realize a reference frame with its origin fixed to center of mass of the Earth system.In this study, GPS (Global Positioning System) observation data from IGS (International GNSS Service) and SLR (Satellite Laser Ranging) tracking data in the period of 2007 to 2016 are applied to estimate the coordinates of IGS sites on Earth’s surface by using the GAMIT/GLOBK and Bernese software. Then, the Helmert transformation model is used to acquire seven parameters between the ITRF (International Terrestrial Reference Frame) reference frame and the CM reference frame. There are three parameters of them are related to the shift in three axes, which are the results of the geocenter motion. Afterwards, the geocenter motion time series are applied with linear fitting method in order to obtain the amplitudes and phases along three axes of geocenter motion.The annual amplitude of X-, Y-, and Z-components between the years 2007 and 2016 are 2.6±0.2mm, 4.1±0.2mm, and 5.6±0.3mm respectively. The annual phase of X-, Y-, and Z-components are 72°, 330°, and 145° respectively. The accuracy of this study is significant improvement comparing to just using GPS or SLR technique only. en_US dc.description.tableofcontents 第一章 緒論 1第一節 研究背景與動機 1第二節 研究目的 3第三節 論文架構 5第二章 文獻回顧 6第一節 地心運動 6一、 前言 6二、 物理機制 8三、 對空間大地測量與地球物理學的影響 11四、 監測方法 13第二節 衛星雷射測距 14一、 系統介紹 14二、 應用部分 15第三章 研究方法與理論基礎 17第一節 實驗流程 18第二節 研究資料及軟體介紹 21一、 資料來源 21二、 軟體介紹 23第三節 SLR觀測量處理 26一、 基礎理論 26二、 坐標反算 29第四節 GPS觀測資料處理 33一、 雙差觀測量計算 35二、 電離層延遲改正 37三、 法方程式解算 41第五節 實驗方法 43第六節 坐標轉換 46第七節 資料擬合 48第四章 實驗成果與分析 49第一節 地心運動時間序列 49一、 僅用GPS測站計算之成果 49二、 僅用SLR測站計算之成果 52三、 合併GPS及SLR測站計算之成果 56第二節 地心運動資料擬合成果 59第五章 結論與建議 69第一節 結論 69一、 僅用GPS測站之研究成果 69二、 僅用SLR測站之研究成果 69三、 合併GPS及SLR測站計算之成果 70四、 地心運動模型擬合成果 70第二節 建議 71參考文獻 73附錄 82 zh_TW dc.format.extent 8175869 bytes - dc.format.mimetype application/pdf - dc.source.uri (資料來源) http://thesis.lib.nccu.edu.tw/record/#G0105257033 en_US dc.subject (關鍵詞) 地心運動 zh_TW dc.subject (關鍵詞) 全球定位系統 zh_TW dc.subject (關鍵詞) 衛星雷射測距 zh_TW dc.subject (關鍵詞) Geocenter motion en_US dc.subject (關鍵詞) Global positioning system (GPS) en_US dc.subject (關鍵詞) Satellite laser ranging (SLR) en_US dc.title (題名) 利用SLR及GPS觀測資料估計地心運動之研究 zh_TW dc.title (題名) The study of using SLR and GPS observation data to estimate geocenter motion en_US dc.type (資料類型) thesis en_US dc.relation.reference (參考文獻) 一、中文參考文獻周旭華、高布錫，2000，「地心的變化及其原因」，『地球物理學報』，43(2)：160-165。謝蘇銳、李斐、鄢建國，2014，「基於空間大地測量與地球物理方法的地心運動研究與監測進展」，『地球物理學進展』，29(1)：15-24。朱文耀、宋淑麗，2010，「國際地球參考框架 (ITRF) 的原點和無整體旋轉」，『天文學進展』，28(4)：321-332。趙德軍、李潭欣、李婧、陳永祥，2015，「DORIS, GPS 和 SLR 空間大地測量技術匯出的地心運動規律」，『測繪工程』，2015(12):21-24。魏娜、施闖、劉經南，2011，「利用GPS資料反演地心運動」，『武漢大學學報資訊科學版』，36(4)：441-445。陳盈樺，2009，「利用測高衛星、重力衛星、NCEP氣候模型估計地心與 C20 變動」，成功大學測量及空間資訊學系碩士論文：台南。二、外文參考文獻Altamimi, Z., Collilieux, X., & Métivier, L., 2011, “ITRF2008: an improved solution of the international terrestrial reference frame”, Journal of Geodesy, 85(8): 457-473.Altamimi, Z., Collilieux, X., Legrand, J., Garayt, B., and Boucher, C., 2007, “ITRF2005: A new release of the International Terrestrial Reference Frame based on time series of station positions and Earth Orientation Parameters”, Journal of Geophysical Research: Solid Earth, 112(B9).Altamimi, Z., Sillard, P., & Boucher, C., 2002, “ITRF2000: A new release of the International Terrestrial Reference Frame for earth science applications”, Journal of Geophysical Research: Solid Earth, 107(B10).Altamimi, Z., Rebischung, P., Métivier, L., & Collilieux, X., 2016, “ITRF2014: A new release of the International Terrestrial Reference Frame modeling nonlinear station motions”, Journal of Geophysical Research: Solid Earth, 121(8): 6109-6131.Argus, D. 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