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Generation of a Bending Angle Radio Occultation Climatology (BAROCLIM) and its use in radio occultation retrievals

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Academic year: 2017

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Table 1. Number of level 1a F3C data provided by UCAR/CDAAC (first column), number of bending angles profiles retrieved at WEGC (second column), and number of profiles, which passed BAROCLIM quality control (last column)
Figure 1. Flowchart of the BAROCLIM generation.
Figure 2. F3C bending angles (in µrad) in January in the latitude band from 80 ◦ S to 90 ◦ S before (top) and after (bottom) the application of the 4σ-outlier rejection criterion
Figure 3. Mean F3C bending angles (in µrad) (top) and their standard deviation (in percent) of the mean (bottom) in January (left) and July (right) as a function of latitude and impact altitude up to 100 km.
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