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    Oceanic Rossby Waves over Eastern Tropical Pacific of Both Hemispheres Forced by Anomalous Surface Winds after Mature Phase of ENSO 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 011:;page 3397
    Author(s): Abe, Hiroto; Tanimoto, Youichi; Hasegawa, Takuya; Ebuchi, Naoto
    Publisher: American Meteorological Society
    Abstract: he present study examined ENSO-related wind forcing contribution to off-equatorial Rossby wave formations in the eastern tropical regions of the North and South Pacific using satellite altimeter data and atmospheric ...
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    Evaluation of Wind Vectors Observed by QuikSCAT/SeaWinds Using Ocean Buoy Data 

    Source: Journal of Atmospheric and Oceanic Technology:;2002:;volume( 019 ):;issue: 012:;page 2049
    Author(s): Ebuchi, Naoto; Graber, Hans C.; Caruso, Michael J.
    Publisher: American Meteorological Society
    Abstract: Wind vectors observed by the QuikSCAT/SeaWinds satellite mission are validated by comparing with wind and wave data from ocean buoys. Effects of oceanographic and atmospheric environment on scatterometer measurements are ...
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    Volume, Heat, and Salt Transports through the Soya Strait and Their Seasonal and Interannual Variations 

    Source: Journal of Physical Oceanography:;2017:;Volume( 047 ):;issue: 005:;page 999
    Author(s): Ohshima, Kay I.; Simizu, Daisuke; Ebuchi, Naoto; Morishima, Shuta; Kashiwase, Haruhiko
    Publisher: American Meteorological Society
    Abstract: olume, heat, and salt transports through the Soya Strait are estimated based on measurements from high-frequency ocean radars during 2003?15 and all available hydrographic data. The baroclinic velocity structure derived ...
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    Wave Dependence of Sea-Surface Wind Stress 

    Source: Journal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 005:;page 705
    Author(s): Toba, Yoshiaki; Iida, Noriko; Kawamura, Hiroshi; Ebuchi, Naoto; Jones, Ian S. F.
    Publisher: American Meteorological Society
    Abstract: Distribution of the wind stress over the oceans is usually estimated by using a bulk formula. It contains the squared 10-m wind speed multiplied by the drag coefficient, which has been assumed in many cases to be a weak ...
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    DSpace software copyright © 2002-2015  DuraSpace
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