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    Thermally Induced Wind Passing from Plain to Basin over a Mountain Range 

    Source: Journal of Applied Meteorology:;1993:;volume( 032 ):;issue: 009:;page 1538
    Author(s): Kimura, Fujio; Kuwagata, Tsuneo
    Publisher: American Meteorological Society
    Abstract: A new concept of a thermally induced local circulation is presented by numerical and observational studies. This wind system transports a low-level air mass from a plain to a basin, passing over a mountain ridge. The ...
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    Daytime Boundary Layer Evolution in a Deep Valley. Part II: Numerical Simulation of the Cross-Valley Circulation 

    Source: Journal of Applied Meteorology:;1997:;volume( 036 ):;issue: 007:;page 883
    Author(s): Kuwagata, Tsuneo; Kimura, Fujio
    Publisher: American Meteorological Society
    Abstract: The thermally induced circulation in a deep valley during fair weather and weak synoptic wind conditions is simulated by a two-dimensional numerical model, in order to investigate the daytime planetary boundary layer ...
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    Heat Budget Analysis of Nocturnal Cooling and Daytime Heating in a Basin 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 019:;page 2917
    Author(s): Kondo, Junsei; Kuwagata, Tsuneo; Haginoya, Shigenori
    Publisher: American Meteorological Society
    Abstract: Nocturnal cooling and daytime heating in a basin were studied on clear and calm days by means of heat budget observations. In the nighttime, drainage flow occurs along the basin sideslope and advects cold air to the boundary ...
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    Numerical Study of the Local Downslope Wind “Hirodo-Kaze” in Japan 

    Source: Monthly Weather Review:;2008:;volume( 136 ):;issue: 001:;page 27
    Author(s): Fudeyasu, Hironori; Kuwagata, Tsuneo; Ohashi, Yukitaka; Suzuki, Shin-ichi; Kiyohara, Yasutomo; Hozumi, Yu
    Publisher: American Meteorological Society
    Abstract: The ?Hirodo-kaze,? a local strong wind accompanying the downslope winds in Japan, is examined using a mesoscale numerical model. The model successfully reproduces the major features of the observed Hirodo-kaze that occurred ...
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