 | Updated: July 2009 The National Hurricane Center (nhc) uses many models as guidance in the preparation of official track and intensity forecasts. The most commonly used models at nhc are summarized in Table 1 150.84 Kb.  1 | read |
| R&D and Alaska’s Natural Environment 11 Approach to Development of a Natural Environmental 11 Senate Joint Resolution (sjr) No. 44 of the Second Session of the 22nd Legislature of the State of Alaska (Appendix A) requested that representative state and federal organizations jointly develop a Research and Development (R&D) plan to 338.85 Kb. 7 | 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 |
| Forced and Unforced Ocean Temperature Changes in Atlantic and Pacific Tropical Cyclogenesis Regions The principal authors discuss the rationale and methods used in the paper “Forced and Unforced Ocean Temperature Changes in Atlantic and Pacific Tropical Cyclogenesis Regions 42.37 Kb. 1 | read |
| Chunzai Wang Pacific wind-forced Kelvin wave, and anomalous zonal advection. These negative feedbacks may work together for terminating El Niño warming, and their relative importance may be time-dependent 2.67 Mb. 15 | read |
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