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    Prevailing Surface Wind Direction during Air–Sea Heat Exchange 

    Source: Journal of Climate:;2019:;volume 032:;issue 017:;page 5601
    Author(s): Ogawa, Fumiaki; Spengler, Thomas
    Publisher: American Meteorological Society
    Abstract: AbstractWhile the climatological-mean sensible and latent heat fluxes are remarkably well described using climatological-mean fields in the bulk flux formulas, this study shows that a significant fraction of the ...
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    Modulations of Storm-Track Activity Associated with the Baroclinic Annular Mode 

    Source: Journal of Climate:;2023:;volume( 036 ):;issue: 012:;page 4219
    Author(s): Nakayama, Morio; Nakamura, Hisashi; Ogawa, Fumiaki
    Publisher: American Meteorological Society
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    Impacts of a Midlatitude Oceanic Frontal Zone for the Baroclinic Annular Mode in the Southern Hemisphere 

    Source: Journal of Climate:;2021:;volume( 034 ):;issue: 018:;page 7389
    Author(s): Nakayama, Morio;Nakamura, Hisashi;Ogawa, Fumiaki
    Publisher: American Meteorological Society
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    Importance of Midlatitude Oceanic Frontal Zones for the Annular Mode Variability: Interbasin Differences in the Southern Annular Mode Signature 

    Source: Journal of Climate:;2016:;volume( 029 ):;issue: 017:;page 6179
    Author(s): Ogawa, Fumiaki; Nakamura, Hisashi; Nishii, Kazuaki; Miyasaka, Takafumi; Kuwano-Yoshida, Akira
    Publisher: American Meteorological Society
    Abstract: midlatitude oceanic frontal zone is a confluent region of warm and cool ocean currents, characterized by a strong meridional gradient in both sea surface temperature (SST) and surface air temperature (SAT). While recent ...
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