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convergence was required to sustain summertime rainfall in monsoon regions, as surface temperatures increase and near-surface relative humidity decreases over land. Possible causes for these changes in the global tropical annual cycle are also being investigated. Dwyer et al. (2012) have examined the possible connections between a projected delay in high-latitude SST, which results from reductions in sea ice, and the delay in the tropical precipitation annual cycle. While high-latitude SST changes were
convergence was required to sustain summertime rainfall in monsoon regions, as surface temperatures increase and near-surface relative humidity decreases over land. Possible causes for these changes in the global tropical annual cycle are also being investigated. Dwyer et al. (2012) have examined the possible connections between a projected delay in high-latitude SST, which results from reductions in sea ice, and the delay in the tropical precipitation annual cycle. While high-latitude SST changes were
, D10108 , doi:10.1029/2005JD006685 . Mantua , N. J. , S. R. Hare , Y. Zhang , J. M. Wallace , and R. C. Francis , 1997 : A Pacific interdecadal climate oscillation with impacts on salmon production . Bull. Amer. Meteor. Soc. , 78 , 1069 – 1079 . Marsland , S. J. , H. Haak , J. H. Jungclaus , M. Latif , and F. Röske , 2003 : The Max-Planck-Institute global ocean/sea ice model with orthogonal curvilinear coordinates . Ocean Modell. , 5 , 91 – 127 . Martin , G
, D10108 , doi:10.1029/2005JD006685 . Mantua , N. J. , S. R. Hare , Y. Zhang , J. M. Wallace , and R. C. Francis , 1997 : A Pacific interdecadal climate oscillation with impacts on salmon production . Bull. Amer. Meteor. Soc. , 78 , 1069 – 1079 . Marsland , S. J. , H. Haak , J. H. Jungclaus , M. Latif , and F. Röske , 2003 : The Max-Planck-Institute global ocean/sea ice model with orthogonal curvilinear coordinates . Ocean Modell. , 5 , 91 – 127 . Martin , G
