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Looks to have three different circulations. Cyclonic low level... to the west of the radar site. Cyclonic Mid level... to the S of the radar. Cyclonic upper level... well to the East of the radar, OR anticyclonic circulation to the west of the radar at upper levels which would be more conducive to strengthening. Top two levels appear to be connected to the remaining flow from the TUTT off to the NW of the system. |