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    Temporal Changes in Some Fresh Water Temperature Structures 

    Source: Journal of Physical Oceanography:;1973:;Volume( 003 ):;issue: 002:;page 226
    Author(s): Lazier, John R. N.
    Publisher: American Meteorological Society
    Abstract: Microstructure is examined in 61 temperature-depth profiles which were obtained at one location in a fresh water lake. Over the 12 hr of observation, specific features of the microstructure are continuous, but increase in ...
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    Migrating Thermal Structure in a Freshwater Thermocline 

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 006:;page 1070
    Author(s): Lazier, John; Sandstrom, Helmuth
    Publisher: American Meteorological Society
    Abstract: The vertical migration of thermal structure in freshwater thermoclines is investigated with theory and observations. The theory is for the wind-forced internal oscillations of a viscous, nonrotating, long narrow lake of ...
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    Convection above the Labrador Continental Slope 

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 004:;page 489
    Author(s): Cuny, Jérôme; Rhines, Peter B.; Schott, Friedrich; Lazier, John
    Publisher: American Meteorological Society
    Abstract: The Labrador Sea is one of the few regions of the World Ocean where deep convection takes place. Several moorings across the Labrador continental slope just north of Hamilton Bank show that convection does take place within ...
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    Observing Deep Convection in the Labrador Sea during Winter 1994/95 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 008:;page 2065
    Author(s): Lilly, Jonathan M.; Rhines, Peter B.; Visbeck, Martin; Davis, Russ; Lazier, John R. N.; Schott, Friedrich; Farmer, David
    Publisher: American Meteorological Society
    Abstract: A 12-month mooring record (May 1994?June 1995), together with accompanying PALACE float data, is used to describe an annual cycle of deep convection and restratification in the Labrador Sea. The mooring is located at ...
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