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    Regional Analysis of Northern Hemisphere 50 kPa Geopotential Heights from 1946 to 1985 

    Source: Journal of Climate:;1990:;volume( 003 ):;issue: 005:;page 543
    Author(s): Shabbar, Amir; Higuchi, Kaz; Knox, John L.
    Publisher: American Meteorological Society
    Abstract: In Knox et al., the interannual variation of the Northern Hemisphere 50 kPa geopotential height field averaged between 30° and 80°N was investigated for the 40-year period from 1946 to 1985. We presented strong statistical ...
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    The Sensitivity of the Simulated Normal and Enhanced C02 Climates to Different Heat Transport Parameterizations in a Two-Dimensional Multilevel Energy Balance Model 

    Source: Journal of Climate:;1995:;volume( 008 ):;issue: 004:;page 844
    Author(s): Chan, Douglas; Higuchi, Kaz; Lin, Charles A.
    Publisher: American Meteorological Society
    Abstract: Atmospheric sensible and latent heat fluxes constitute an important component of the total poleward energy transport in the climate system. The authors investigate the relative role of these heat fluxes in normal and ...
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    Secular Variation of Northern Hemisphere 50 kPa Geopotential Height 

    Source: Journal of Climate:;1988:;volume( 001 ):;issue: 005:;page 500
    Author(s): Knox, John L.; Higuchi, Kaz; Shabbar, Amir; Sargent, Neil E.
    Publisher: American Meteorological Society
    Abstract: There is accumulating evidence in the literature that different short-period climate regimes (subclimates) may have characterized the Northern Hemisphere during the past 40 years. We, therefore, investigate the 40-yr record ...
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    Modeling and Scaling Coupled Energy, Water, and Carbon Fluxes Based on Remote Sensing: An Application to Canada’s Landmass 

    Source: Journal of Hydrometeorology:;2007:;Volume( 008 ):;issue: 002:;page 123
    Author(s): Chen, Baozhang; Chen, Jing M.; Mo, Gang; Yuen, Chiu-Wai; Margolis, Hank; Higuchi, Kaz; Chan, Douglas
    Publisher: American Meteorological Society
    Abstract: Land surface models (LSMs) need to be coupled with atmospheric general circulation models (GCMs) to adequately simulate the exchanges of energy, water, and carbon between the atmosphere and terrestrial surfaces. The ...
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