InSAR に含まれる対流圏伝搬遅延 : ノイズの場合と ... - 北海道大学

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Fig 20. Estimated dTEC model from azimuth offset field shown in Figure 18. 35
36 a [rad] A B b [rad] A B Fig 21. (a) Observed interferogram (same as Figure 13, but different scale). (b) “dTEC” corrected interferogram.
Page 1 and 2: InSAR に含まれる対流圏
Page 3 and 4: 2 Method 1 による遅延量
Page 5 and 6: 4 1. はじめに 1.1 衛星測
Page 7 and 8: 6 1.2.2 InSAR SAR のデータを
Page 9 and 10: 8 れてしまうため InSAR で
Page 11 and 12: 10 (2) 式の右辺第 2 項
Page 13 and 14: 12 2. 高分解能数値気
Page 15 and 16: 14 2.3 KARAT KARAT (Kashima Ray-Tra
Page 17 and 18: 16 2.4.2 calibration 法による
Page 19 and 20: 18 本論文ではこの補正
Page 21 and 22: 20 因による位相変化
Page 23 and 24: 22 Table 2. Root Mean Square residu
Page 25 and 26: 24 2.6 結論我々は KARAT と
Page 27 and 28: 26 Fig 11. (left) Surface weather m
Page 29 and 30: 28 Fig 13. Unwrapped SAR interferog
Page 31 and 32: 30 Fig 15. Interferogram for 23 Oct
Page 33 and 34: 32 3.2.3 電離層の擾乱
Page 35: 34 B Fig 18. Azimuth offset field w
Page 39 and 40: 38 [rad] [rad] Fig 23. (top) Observ
Page 41 and 42: 40 3.3 calibration 法による
Page 43 and 44: Fig 26. Estimated tropospheric phas
Page 45 and 46: 44 3.3.2 結果の考察 Figure
Page 47 and 48: 46 [mm] Fig 29. InSAR image (same a
Page 49 and 50: 48 5. 謝辞まず初めに本
Page 51 and 52: 50 藤原智・飛田幹男
Page 53: 52 http://www.mmm.ucar.edu/wrf/user

InSAR に含まれる対流圏伝搬遅延 : ノイズの場合と ... - 北海道大学

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