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The Entrainment Influence on the Ocean Surface Layer in Tropical Latitudes
Entrainment Influence Tropical Latitudes Ocean Surface Layer
2009/3/9
A nonlinear, time-dependent, baroclinic model is developed for a zonally uniform, tropical, two-layer ocean on a north-south vertical section. The lower layer is infinitely deep, at rest, and at const...
A Calculation of Ocean Heat Storage and Effective Ocean Surface Layer Depths for the Northern Hemisphere
Ocean Heat Storage Ocean Surface Layer Depths Northern Hemisphere
2009/1/21
In the hierarchy of simple ocean formulations available for coupling to atmospheric GCMs, a scheme whereby ocean surface-layer depths vary geographically and seasonally is deemed better than a fixed d...
Modeling Wave-Enhanced Turbulence in the Ocean Surface Layer
Wave-Enhanced Turbulence Ocean Surface Layer
2008/12/17
Until recently, measurements below the ocean surface have tended to confirm “law of the wall” behavior, in which the velocity profile is logarithmic, and energy dissipation decays inversely with depth...
Turbulence Decay and Restratification in the Equatorial Ocean Surface Layer following Nighttime Convection
Nighttime Convection Turbulence Decay Equatorial Ocean Surface Layer
2008/11/18
Although the process of restratification of the ocean surface layer at the equator following nighttime convection is similar in many ways to the process at midlatitudes, there are important difference...