A Velocity Dealiasing Scheme Based on Minimization of Velocity Differences between Regions

Figure 7

(a) The vector wind fields from the ERA-Interim at 900 hPa at 15:00 UTC on September 14, 2016. The radial velocity field of 0.5° elevation observed by Xiamen radar at 14:59 UTC, September 14, 2016: (b) raw velocity field, (c) manually dealiased velocity field, (d) dealiased velocity field by the CIDA algorithm, and (e) dealiased velocity field by the MVDR algorithm. The manual dealiased results are marked by white ellipses in (c).

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