第六章 結論與建議
第二節 建議
國
立 政 治 大 學
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N a tio na
l C h engchi U ni ve rs it y
三、不同來源資料改正對流層總延遲量，可獲得良好改正成果
以較佳的兩組改正成果像對 I 及像對 III 來討論，由數據可發現在對流 層總改正當中，像對 I 為乾加濕總改正較佳，而像對 III 中以 Niell 模式總 改正較佳。可得出兩種方式皆可有效改正大氣效應，在執行大氣改正時，
皆可嘗試，並獲取較好之地表變形成果。
第二節 建議
依據對 SAR 之認知以及大氣改正研究處理方面，給出以下建議：
一、採用不同之 SAR 衛星影像
本研究採用之 SAR 影像為 PALSAR 影像，而 SAR 影像有 ERS、ASAR、
COSMO-SkyMed（COnstellation of small Satellites for the Mediterranean basin Observation）等多種不同波段影像，建議未來可採取其它影像作研究。
二、採用不同之大氣模式
處理大氣改正過程中，採用之濕改正資料來源為 WRF 模型。目前有的 大氣模型眾多，諸如 GAM、ECMWF 等，可依地區特性以不同大氣模型執 行改正。
三、電離層改正
本研究主要著重於對流層之改正，電磁波在大氣中行進亦會受到電離 層影響，因此建議未來可深入探討電離層延遲量改正對於 SAR 之影響。
‧
謝嘉聲、史天元，2001，「以 Doris 進行雷達差分干涉技術產生數值地形模 型之研究」，論文發表於〈第二十屆測量學術及應用研討會〉，國立中央大 學太空及遙測研究中心：中壢市，2001 年 9 月 6 日至 7 日。
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