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Aaron B. Wilson, David H. Bromwich, and Keith M. Hines

upper boundary pressure surface (~3 hPa). Modifications to the convective momentum transport and a convective available potential energy dilution approximation have improved intraseasonal variability and weakened model trade winds, allowing for a better representation of ENSO ( Hurrell et al. 2006 ; Neale et al. 2008 ). b. CAM simulation strategy The four main regions in the tropical Pacific Ocean monitored for the development of ENSO are as follows (from west to east): Niño-4 (5°N–5°S, 160°E–150°W

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