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Impact of resolving the diurnal cycle in an ocean-atmosphere GCM. Part 2: A diurnally coupled CGCM.

By D.J. Bernie, E. Guilyardi, G. Madec, J.M. Slingo, S.J. Woolnough and J. Cole
Topics: 530, 551
Publisher: Springer
Year: 2008
OAI identifier: oai:centaur.reading.ac.uk:1198

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Citations

  1. (2007). Impact of resolving the diurnal cycle in an ocean-atmosphere GCM. Part 1: Diurnally forced OGCM. Clim Dyn 29:575–590
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  3. (1998). Intraseasonal variability of surface fluxes and sea surface temperatures in the tropical western Pacific and Indian oceans.
  4. (2000). Rectification of the Madden–Julian oscillation into the ENSO cycle.
  5. (1996). Surface buoyancy forcing and the mixed layer of the western Pacific warm pool: observations and 1D model results.
  6. (2004). Wave breaking and ocean surface layer thermal responce. J Phys Oceanogr 34:693–698 (notes and Correspondants) Nakazawa T

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