 | P. O. Box 3000 Boulder, co, 80307-3000 The variability of ssts in the tropical Atlantic is well represented in ccsm4 although the leading eof in ccsm4 shows more homogeneous warming than the leading eof in observations 3.04 Mb.  16 | read |
| Tropical Atlantic Oceanic Variability in the ccsm4 Ernesto Muñoz Benguela region indicates that the variability of ssts is dominated by vertical advection. The subtropical waters in the coupled configuration reach the Equator mainly from the South Atlantic 2.12 Mb. 6 | read |
 | North Atlantic Gyre Circulation Variability Associated with the Atlantic Multidecadal Oscillation Yanyun Liu1,2, Sang-Ki Lee1,2, Barbara A. Muhling3, John T. Lamkin3, David B. Enfield1,2, Chunzai Wang2, Christopher S. Meinen2 and Molly O. Baringer2 48.03 Kb. 1 | read |
| Precipitation from African Easterly Waves Itcz and its seasonal migration improves in the higher-resolution case. This suggests that capturing these transient waves and the resultant strong low-level convergence is one of the key ingredients for improving the simulation of precipitation in global 6.72 Mb. 4 | read |
| Intertropical Convergence Zone in the South Atlantic and the equatorial cold tongue The result is a zonal band of surface wind convergence that exceeds 10-6 1/s, rainfall stronger than 2 mm/day, and an associated decrease in ocean surface salinity of 2 ppt 0.49 Mb. 7 | read |
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