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    Three-Dimensional Effects in Flow over Mountains 

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 006:;page 1223
    Author(s): Wong, K. K.
    Publisher: American Meteorological Society
    Abstract: An investigation is made of three-dimensional effects on the flow upstream of a mountain whose shape varies in a horizontal direction transverse to the wind. To generate the mountain, a dipole whose strength varies ...
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    Dependence of Rainfall Variability on Mean Rainfall, Latitude, and the Southern Oscillation 

    Source: Journal of Climate:;1990:;volume( 003 ):;issue: 001:;page 163
    Author(s): Nicholls, N.; Wong, K. K.
    Publisher: American Meteorological Society
    Abstract: The relationship between the relative variability of annual rainfall, the long-term mean annual rainfall, the latitude, and the correlation between annual rainfall and the Southern Oscillation Index is examined, using data ...
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    Mesoscale Perturbations on Airflow in the Urban Mixing Layer 

    Source: Journal of Applied Meteorology:;1978:;volume( 017 ):;issue: 005:;page 677
    Author(s): Wong, K. K.; Dirks, R. A.
    Publisher: American Meteorological Society
    Abstract: Urban perturbations on the mixing layer airflow over St. Louis were studied as a part of METROMEX. Case studies were conducted on summer days under generally undisturbed synoptic weather conditions. Based on simultaneous ...
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    Reply 

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 004:;page 773
    Author(s): Wong, K. K.; Kao, Timothy W.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Stratified Flow over Extended Obstacles and Its Application to Topographical Effect on Vertical Wind Shear 

    Source: Journal of the Atmospheric Sciences:;1970:;Volume( 027 ):;issue: 006:;page 884
    Author(s): Wong, K. K.; Kao, Timothy W.
    Publisher: American Meteorological Society
    Abstract: An investigation is made of the two-dimensional flow of a stratified fluid over an extended obstacle, characterized by a source disturbance, for an infinite medium and for a layer of finite depth. The problems are posed ...
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