 | Tropical cyclones: Formation and Decay by Steve Graham and Holli Riebeek · November 1, 2006 Called the greatest storm on Earth, a hurricane is capable of annihilating coastal areas with sustained winds of 155 miles per hour or higher, intense areas of rainfall, and a storm surge 41.78 Kb.  1 | read |
 | Application of a Hybrid Dynamical–Statistical Model for Week 3 to 4 Forecast of Atlantic/Pacific Tropical Storm and Hurricane Activities 107.35 Kb. 1 | read |
| J. W. Hurrell National Center for Atmospheric Research Nao, in particular a change in the boreal winter atmospheric circulation toward enhanced middle latitude westerly flow (the positive nao index phase). But what about changes in the Atlantic climate during other times of the year? 21.57 Kb. 1 | read |
| Application of a Hybrid Dynamical–Statistical Model for Week 3 to 4 Forecast of Atlantic/Pacific Tropical Storm and Hurricane Activities 410.3 Kb. 4 | read |
| 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 |
| 20. Arc Cloud Module Principal Investigator: Jason Dunion Links to ifex: Goal 1 Goal 1: Collect observations that span the tc life cycle in a variety of environments for model initialization and evaluation 170.37 Kb. 1 | 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 |
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