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An Evaluation of Positioning Error Estimated by the Mesoscale Non-Hydrostatic Model

a. c. b. wind. Figure 1 (a) Study area (b) Topography of the study area (c) Cloud images of the study area retrieved by the GMS. Atmospheric mountain waves are excited on the leeward side of the mountains[Shimada et al., 2002]. Radio Source (QSO or GPS Satellite). Figure 3

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An Evaluation of Positioning Error Estimated by the Mesoscale Non-Hydrostatic Model