Titlebook: Climate-Ocean Interaction; M. E. Schlesinger Book 1990 Kluwer Academic Publishers 1990 Ocean.Scale.Sea ice.satellite.temperature

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https://doi.org/10.1007/978-3-662-46888-3ure anomaly fields in four recent decades are provided, and likely future improvements to this new analysis are outlined. The combined analyses are now making it possible to compare comprehensively changes in global and regional surface temperature observed in recent decades with numerical predictio

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Risikokompetenz und deren Hemmnissetential density increment in the Southern Ocean are in reasonable accord with observations. When the amount of sea ice freezing is expressed as a function of hemispheric mean sea surface temperature (calibrated from the seasonal cycle), the model predicts the possible cutoff of AABW and most of the

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Book 1990es of Decades to Centuries, and Impact of Paleoclimatic Proxy Data on Climate Modelling. Preface ix Acknowledgements I thank Howard Cattle and Neil Wells for their guidance and assistance as members of the Workshop Organizing Committee. I particularly thank Michael Davey for all his efforts as Local