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    Comments on "Coastal Trapped Waves in a Stratified Ocean" 

    Source: Journal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 004:;page 773
    Author(s): Mysak, L. A.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    On the Damping of Second-Class Trapped Waves on a Sloping Beach 

    Source: Journal of Physical Oceanography:;1982:;Volume( 012 ):;issue: 012:;page 1527
    Author(s): Hukuda, H.; Mysak, L. A.
    Publisher: American Meteorological Society
    Abstract: The effect of linear bottom friction on free topographic (second class) waves on a sloping beach is investigated. To handle the coastal singularity in the friction terms, Lighthill's method of strained coordinates is used ...
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    Present-Day and Last-Glacial-Maximum Ocean Thermohaline Circulation in a Zonally Averaged Coupled Ocean–Sea-Ice–Atmosphere Model 

    Source: Journal of Climate:;2001:;volume( 014 ):;issue: 007:;page 1422
    Author(s): Bjornsson, H.; Mysak, L. A.
    Publisher: American Meteorological Society
    Abstract: A simple ocean?atmosphere model suitable for long-term paleoclimate studies is presented. It consists of a three-basin zonally averaged ocean model coupled to an energy moisture-balance atmospheric model and a thermodynamic ...
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    Edge Waves in the Presence of an Irregular Coastline 

    Source: Journal of Physical Oceanography:;1977:;Volume( 007 ):;issue: 006:;page 846
    Author(s): Fuller, J. D.; Mysak, L. A.
    Publisher: American Meteorological Society
    Abstract: We examine the generation of trapped edge waves on a continental shelf when a long wave from the deep ocean reaches an irregular coast, and alterations in the propagation characteristics of trapped edge waves due to the ...
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    The Scattering of Rossby Waves by a Semi-Infinite Barrier 

    Source: Journal of Physical Oceanography:;1972:;Volume( 002 ):;issue: 001:;page 108
    Author(s): Mysak, L. A.; LeBlond, P. H.
    Publisher: American Meteorological Society
    Abstract: We discuss the scattering of divergent Rossby waves by a semi-infinite vertical barrier of arbitrary orientation on a ? plane. The Wiener-Hopf method is used to obtain an integral representation of the scattered wave field ...
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    Atmospherically Forced Eddies in the Northeast Pacific 

    Source: Journal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 011:;page 1769
    Author(s): Willmott, A. J.; Mysak, L. A.
    Publisher: American Meteorological Society
    Abstract: In the northeast Pacific eddies are observed in the salinity and, to a lesser extent, in the thermal anomalies. In particular, a pronounced eddy is frequently observed a few hundred kilometers west of Sitka, Alaska, latitude ...
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    Modeling Sea Ice as a Granular Material, Including the Dilatancy Effect 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 011:;page 2342
    Author(s): Tremblay, L-B.; Mysak, L. A.
    Publisher: American Meteorological Society
    Abstract: A dynamic sea ice model based on granular material rheology is presented. The sea ice model is coupled to both a mixed layer ocean model and a one-layer thermodynamic atmospheric model, which allows for an ice albedo ...
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    Evidence for a 40–60 Day Oscillation over the Western Indian Ocean during 1976 and 1979 

    Source: Monthly Weather Review:;1984:;volume( 112 ):;issue: 002:;page 383
    Author(s): Mertz, G. J.; Mysak, L. A.
    Publisher: American Meteorological Society
    Abstract: Surface wind data for the western region of the Indian Ocean was collated at the University of Miami, in support of certain FGGE/INDEX/MONEX projects, and published in two technical reports by Fernandez-Partagas and Düing ...
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    A Note on “Internal Waves in a Randomly Stratified Fluid” 

    Source: Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 002:;page 243
    Author(s): Tang, C. L.; Mysak, L. A.
    Publisher: American Meteorological Society
    Abstract: We show that in the presence of a randomly perturbed stability frequency, a coherent internal wave (f<σ<N0) or gyroscopic wave (N0<σ<f) is always attenuated in the direction of energy propagation, where σ and f denote ...
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    A Numerical Simulation of Sea Ice Cover in Hudson Bay 

    Source: Journal of Physical Oceanography:;1994:;Volume( 024 ):;issue: 012:;page 2515
    Author(s): Wang, Jia; Mysak, L. A.; Ingram, R. G.
    Publisher: American Meteorological Society
    Abstract: Hibler's dynamic-thermodynamic sea ice model with viscous-plastic rheology is used to simulate the seasonal cycle of sea ice motion, thickness, compactness, and growth rate in Hudson Bay under monthly climatological ...
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