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Synoptic-scale Mesoscale Environments Conducive to Forest Fires During the October 2003 Extreme Fire Event in Southern California

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Figure

Fig. 3: North American Regional Reanalysis (NARR)-A of 300 hPa geopotential height
Fig. 4: 300 hPa convergence (10-5observational data valid at (a) 1200 UTC 25, (b) 0000 UTC 26 and (c) 1200 UTC 26  s-1) derived from Barnes analyses of radiosonde October 2003
Fig. 5: Schematics of the dynamics of a (a) straight jet streak, (b) highly anticyclonically curved jet stream (shaded without along stream wind speed maximum) and (c) highly anticyclonically curved jet streak
Fig. 5 (Continued)
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