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In this analysis, we examine the lower tropospheric stability in CAM4 and CAM5. The lower tropospheric stability is examined across the Arctic domain with analysis products, and in more detail using in-situ data at the North Slope of Alaska.

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There is no significant difference between the southern part and the northern part of EAL in the percentages of SST contribution.

The remote SST anomalies regulates rainfall over EAL probably by modulating the horizontal water vapor transport rather than the vertical motion, since the horizontal water vapor transport into EAL is strongly modulated by SST but the vertical motion over EAL is not.