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    Ocean Surface Drift Velocities 

    Source: Journal of Physical Oceanography:;1977:;Volume( 007 ):;issue: 004:;page 606
    Author(s): Kraus, E. B.
    Publisher: American Meteorological Society
    Abstract: Symmetry considerations indicate that in steady-state conditions, and in the absence of a sea current, a horizontal interface must move in the direction of the surface geostrophic wind. With currents present, the interface ...
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    The Diurnal Precipitation Change over the Sea 

    Source: Journal of the Atmospheric Sciences:;1963:;Volume( 020 ):;issue: 006:;page 551
    Author(s): Kraus, E. B.
    Publisher: American Meteorological Society
    Abstract: Analysis of nine weathership records indicates that maritime precipitation is significantly more frequent at night. The effect varies with season and latitude. The diurnal variation is related to the absorption of solar ...
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    The Aerodynamic Roughness of the Sea Surface 

    Source: Journal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 004:;page 443
    Author(s): Kraus, E. B.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    The Bahama Bank Planetary Boundary Layer Experiment April– May 

    Source: Bulletin of the American Meteorological Society:;1971:;volume( 052 ):;issue: 010:;page 969
    Author(s): Kraus, E. B.
    Publisher: American Meteorological Society
    Abstract: A field program to study the marine planetary boundary layer was carried out jointly by scientists and students from the Universities of British Columbia, Hamburg and Miami and by personnel from the NOAA Sea-Air Interaction ...
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    Subtropical Droughts and Cross-Equatorial Energy Transports 

    Source: Monthly Weather Review:;1977:;volume( 105 ):;issue: 008:;page 1009
    Author(s): Kraus, E. B.
    Publisher: American Meteorological Society
    Abstract: The spatial coherence of subtropical rainfall anomalies is documented by variance analysis. Major droughts repeatedly were felt at the same time around the globe along the arid margins of the tropical rainfall belt. The ...
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    The Seasonal Excursion of the Intertropical Convergence Zone 

    Source: Monthly Weather Review:;1977:;volume( 105 ):;issue: 008:;page 1052
    Author(s): Kraus, E. B.
    Publisher: American Meteorological Society
    Abstract: A simple analytical model relates the seasonal excursion of the Intertropical Convergence Zone to seasonal changes in hemispheric forcing. The maximum value of the excursion increases with the seasonal heating change; it ...
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    Numerical Experiments with Large-Scale Seasonal Forcing 

    Source: Journal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 001:;page 3
    Author(s): Kraus, E. B.; Lorenz, E. N.
    Publisher: American Meteorological Society
    Abstract: Experiments with six different heating fields in a numerical general circulation model are described. Three different vertical heating gradients are each used once with and once without variations on the continental-oceanic ...
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