 | A unified Modeling Approach to Climate System Prediction James Hurrell* 1, Gerald A. Meehl 1, David Bader 2 Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, fl and 82.14 Kb.  1 | read |
 | El Nino Arrives in 2015 Pacific and is often brought about by subsiding trade winds and maximum sunlight. The sea surface waters heat up and the heat is transferred to the atmosphere above as the sea water moves east to west 1.06 Mb. 13 | read |
| Prediction from Weeks to Decades Ben Kirtman, David Anderson, Gilbert Brunet, In-Sik Kang, Adam Scaife and Doug Smith 206.63 Kb. 3 | 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 |
| Prediction from Weeks to Decades Decadal Variability (amv); trend among others. Some of the outstanding challenges include how to evaluate and validate prediction systems, how to improve models and prediction systems 1.43 Mb. 6 | read |
| High Resolution Model Intercomparison Project (HighResmip) R. J. Haarsma C. A. Senior2, A. Bellucci4, S. Corti5, N. S. Fučkar6, V. Guemas6, J. von Hardenberg5, W. Hazeleger1,7,8, C. Kodama9, T. Koenigk10, L. R. Leung11, J. Lu11, J. J. Luo12, J. Mao13, M. S. Mizielinski2, R 286.15 Kb. 2 | read |
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