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    Eddy Heat Fluxes and Stability of Planetary Waves. Part I 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 011:;page 2353
    Author(s): Lin, Charles A.
    Publisher: American Meteorological Society
    Abstract: The stability of baroclinic Rossby waves in a zonal shear flow is examined. The model used is a linear, quasi-geostrophic, two-level, adiabatic and frictionless midlatitude ?-plane model. The perturbations consist of ...
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    Eddy Heat Fluxes and Stability of Planetary Waves. Part II 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 011:;page 2373
    Author(s): Lin, Charles A.
    Publisher: American Meteorological Society
    Abstract: The stability analysis of baroclinic Rossby waves in a zonal shear flow examined in Part I is applied to the atmosphere. The basic state consists of a planetary-scale (wavenumber 1) Rossby wave in a zonal flow with vertical ...
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    The Effect of Nonlinear Diffusive Heat Transport in a Simple Climate Model 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 002:;page 337
    Author(s): Lin, Charles A.
    Publisher: American Meteorological Society
    Abstract: The effects of nonlinear diffusive beat transport in North's (1975) model is reexamined. By inserting the nonlinearity into the original energy balance equation rather than the spectrally transformed linear algebraic ...
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    The Adaptive Spectral Element Method and Comparisons with More Traditional Formulations for Ocean Modeling 

    Source: Journal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 001:;page 135
    Author(s): Dupont, Frédéric; Lin, Charles A.
    Publisher: American Meteorological Society
    Abstract: Triangular spectral elements offer high accuracy in complex geometries, but solving the related matrix problem can be cumbersome and time consuming. In restricted applications, recent developments have led to a family of ...
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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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    Mesoscale Circulations Forced by Melting Snow. Part II: Application to Meteorological Features 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 011:;page 1642
    Author(s): Szeto, Kit K.; Stewart, Ronald E.; Lin, Charles A.
    Publisher: American Meteorological Society
    Abstract: Various authors have proposed that the cooling associated with melting precipitation contributes significantly to the dynamics of mesoscale precipitation systems. In this study, we use the numerical model described in Part ...
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    Mesoscale Circulations Forced by Melting Snow. Part I: Basic Simulations and Dynamics 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 011:;page 1629
    Author(s): Szeto, Kit K.; Lin, Charles A.; Stewart, Ronald E.
    Publisher: American Meteorological Society
    Abstract: The melting of snow extracts latent heat of fusion from the environment. The basic response of the atmosphere to this cooling-by-melting mechanism is investigated by using a nonlinear two-dimensional numerical model. It ...
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    Observational Study of Wind Channeling within the St. Lawrence River Valley 

    Source: Journal of Applied Meteorology and Climatology:;2009:;volume( 048 ):;issue: 011:;page 2341
    Author(s): Carrera, Marco L.; Gyakum, John R.; Lin, Charles A.
    Publisher: American Meteorological Society
    Abstract: The presence of orography can lead to thermally and dynamically induced mesoscale wind fields. The phenomenon of channeling refers to the tendency for the winds within a valley to blow more or less parallel to the valley ...
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    A Reexamination of the polar Halocline Catastrophe and Implications for Coupled Ocean-Atmosphere Modeling 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 002:;page 287
    Author(s): Zhang, Sheng; Greatbatch, Richard J.; Lin, Charles A.
    Publisher: American Meteorological Society
    Abstract: In this paper, the physical mechanism of the polar halocline catastrophe (PHC) is reexamined with emphasis on the role played by the surface heat flux. It is argued that, in a coupled ocean?atmosphere system, thermal changes ...
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    A Semi-implicit Semi-Lagrangian Finite-Element Shallow-Water Ocean Model 

    Source: Monthly Weather Review:;2000:;volume( 128 ):;issue: 005:;page 1384
    Author(s): Le Roux, Daniel Y.; Lin, Charles A.; Staniforth, Andrew
    Publisher: American Meteorological Society
    Abstract: The finite-element, semi-implicit, and semi-Lagrangian methods are combined together to solve the shallow-water equations using unstructured triangular meshes. Triangular finite elements are attractive for ocean modeling ...
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