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    The Heat Content of the Upper Ocean During Coastal Upwelling: Oregon, August 1973 

    Source: Journal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 002:;page 379
    Author(s): Reed, R. K.; Halpern, D.
    Publisher: American Meteorological Society
    Abstract: Data obtained at a time-series station during intense coastal upwelling off Oregon were applied to a model of heat conservation for the upper 8 m, and a thermal eddy diffusivity (horizontal) of 300 M2s?1 was computed. ...
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    Correlation of Current and Sea Level in the Eastern Equatorial Pacific 

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 004:;page 811
    Author(s): Hayes, S. P.; Halpern, D.
    Publisher: American Meteorological Society
    Abstract: Upper-ocean current and temperature records from neat 0°, 110°W are compared with Galapagos Island sea level measurements (0°3?S, 91°28?W) for the period March 1980 to July 1981. Low-frequency (periods greater than 30 days) ...
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    Comparison of Shipboard Acoustic Doppler Current Profiler and Moored Current Measurements in the Equatorial Pacific 

    Source: Journal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;issue: 004:;page 742
    Author(s): Chereskin, T. K.; Halpern, D.; Regier, L. A.
    Publisher: American Meteorological Society
    Abstract: Depth-averaged current shears computed from shipboard acoustic Doppler current profiler (ADCP) and moored Savonius rotor and vane vector-averaging current meter (VACM) measurements are compared at 35, 62.5, 100 and 140 m ...
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    Vertical Structure of Low Frequency Variability in the Eastern Equatorial Pacific Ocean 

    Source: Journal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 007:;page 1009
    Author(s): Tang, T. Y.; Weisberg, R. H.; Halpern, D.
    Publisher: American Meteorological Society
    Abstract: The vertical structure of low frequency velocity and temperature variability in the eastern equatorial Pacific Ocean is examined using surface and subsurface moored current meter data from 0°, 110°W between 20 and 3027 m ...
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    Comparison of Observed and Model Wind Velocities 

    Source: Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 003:;page 314
    Author(s): Pazan, S. E.; Barnett, T. P.; Tubbs, A. M.; Halpern, D.
    Publisher: American Meteorological Society
    Abstract: The global band wind analysis produced by the Fleet Numerical Oceanography Center (FNOC) has been compared with direct buoy observations of winds in the Central Equatorial Experiment. Using the six months of available data ...
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    Why the ITCZ Is Mostly North of the Equator 

    Source: Journal of Climate:;1996:;volume( 009 ):;issue: 012:;page 2958
    Author(s): Philander, S. G. H.; Gu, D.; Lambert, G.; Li, T.; Halpern, D.; Lau, N-C.; Pacanowski, R. C.
    Publisher: American Meteorological Society
    Abstract: Although the distribution of sunshine is symmetrical about the equator, the earth's climate is not. Climatic asymmetries are prominent in the eastern tropical Pacific and Atlantic Oceans where the regions of maximum sea ...
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