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Storm Track Sensitivity to Resolution and Climate Change in High-Resolution Global Simulations.

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Figure

Figure 3.1: The average wintertime (DJF) local deepening rate (LDR), measured in hPa/day, over the 26-year period from 1985-2011 for a) UPSCALE 130km, b) UPSCALE 60km, c) UPSCALE 25km, over the 10-year period for c) MPAS 15km, and d) the climatological mea
Figure 3.2: The climate warming differences (future minus current) of the average wintertime LDR, measured in hPa/day, for UPSCALE a) 130km and b) 25km is shaded below circular hatching that shows where all ensemble members (5 for 130km, 3 for 25km) agree
Figure 3.3: The resolution differences, higher (25km) minus lower (130km), of the average wintertime LDR for a) present and b) future UPSCALE simulations, with units hPa/day
Figure 3.4: The precipitation rate covariance with the local deepening rate for UPSCALE present a) 130km in the West Atlantic, b) 130km in the East Atlantic, c) 25km in the West Atlantic, and d) 25km in the East Atlantic
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