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WRF summer extreme daily precipitation over the CORDEX Arctic

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Figure

Figure 1. CORDEX Arctic 50 km domain with the North American analysis regions.
Figure 2. Pan-Arctic WRF-ERA Interim reanalysis 16 year JAS (a) mean sea level pressure bias (hPa), (b) 500 hPa geopotential height bias (geopotential meters), and (c) 2 m speci fic humidity bias (kg kg 1 ).
Figure 3. Frequency versus intensity distribution of Pan-Arctic WRF ensemble and NCDC station observations for (a) Canada East and (b) Canada West
Figure 3 shows daily precipitation ’s pooled 16 year frequency versus intensity for each analysis region
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