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    Loss of Hyperbolicity and Ill-posedness of the Viscous–Plastic Sea Ice Rheology in Uniaxial Divergent Flow 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 011:;page 2920
    Author(s): Gray, J. M. N. T.
    Publisher: American Meteorological Society
    Abstract: Local contact interactions between sea ice floes can be modeled on the large scale by treating the pack as a two-dimensional continuum with granular properties. One such model, which has gained prominence, is the viscous ...
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    Isotopes in Precipitation in Northwestern North America 

    Source: Monthly Weather Review:;1975:;volume( 103 ):;issue: 011:;page 958
    Author(s): Hage, K. D.; Gray, J.; Linton, J. C.
    Publisher: American Meteorological Society
    Abstract: Regional analyses of oxygen and deuterium isotope abundances in precipitation from selected stations of the International Atomic Energy Agency-World Meteorological Organization global netwok are presented as background for ...
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    Reply 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 003:;page 482
    Author(s): Gray, J. M. N. T.; Killworth, Peter D.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    Sea Ice Ridging Schemes 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 011:;page 2420
    Author(s): Gray, J. M. N. T.; Killworth, Peter D.
    Publisher: American Meteorological Society
    Abstract: As sea ice is advected on the surface of the ocean, the ice concentration (0 ≤ A ≤ 1) and the mean ice thickness change in response to thermodynamic and mechanical forcing. In this paper the authors review the existing ...
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    Stability of the Viscous-Plastic Sea Ice Rheology 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 005:;page 971
    Author(s): Gray, J. M. N. T.; Killworth, Peter D.
    Publisher: American Meteorological Society
    Abstract: The large-scale two-dimensional rheology of a sea ice pack arises from the local contact forces between adjacent does in convergence. It is conventionally modeled by a viscous-plastic constitutive relation to reflect the ...
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