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    A Consistent Model for the Large-Scale Steady Surface AtmosphericCirculation in the Tropics 

    Source: Journal of Climate:;1999:;volume( 012 ):;issue: 010:;page 2956
    Author(s): Battisti, David S.; Sarachik, E. S.; Hirst, A. C.
    Publisher: American Meteorological Society
    Abstract: The authors present a new model of the tropical surface circulation, forced by changes in sensible heat and evaporative flux anomalies that are associated with prescribed sea surface temperature anomalies. The model is ...
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    Why Does the Indonesian Throughflow Appear to Originate from the North Pacific? 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 006:;page 1087
    Author(s): Godfrey, J. S.; Wilkin, J.; Hirst, A. C.
    Publisher: American Meteorological Society
    Abstract: Most available wind products show a mean wind stress curl across the Pacific at 2°N that is close to zero, so a Sverdrup model predicts the western boundary current at the Asian coast to be nearly zero at this latitude. ...
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    Thermal Expansion in Ocean and Coupled General Circulation Models 

    Source: Journal of Climate:;2000:;volume( 013 ):;issue: 008:;page 1384
    Author(s): Jackett, D. R.; McDougall, T. J.; England, M. H.; Hirst, A. C.
    Publisher: American Meteorological Society
    Abstract: More than half of the predicted rise in future sea level caused by the enhanced greenhouse effect is currently thought to be due to the thermal expansion of the oceans. Here methods for quantifying this thermal expansion ...
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    DSpace software copyright © 2002-2015  DuraSpace
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