WebDue to the thermobaric effect, stirring, or exchanging water masses, along isopycnal surface is associated with the change of GPE in the mean state. This is a new type of instability, called the thermobaric instability. In addition, due to cabbeling subscale diffusion of water parcels always leads to the release of GPE. WebApr 1, 2024 · Effects of eddies on the subduction and movement of water masses reaching the $$137^{\circ }\,\hbox {E}$$ section using Lagrangian particles in an eddy-resolving OGCM ... Role of parameterized eddies in the energy budget of the global thermohaline circulation: cabbeling versus restratification. Journal of Physical Oceanography 2010 …
L. Shogo Urakawa Japan Meteorological Agency 17 Publications …
WebDue to the cabbeling effect, these density gradients are increasingly dominated by temperature gradients in a warming ocean, and a direct link exists between North Atlantic mean temperature and ... Webthe volume contraction, cabbeling affects potential en-ergy and so could affect dynamics and enhance mixing [see a recent contribution by Fofonoff (1995, 1998) for the Gulf … ez0729
Kinetic energy transfers between mesoscale and submesoscale …
http://oceans.mit.edu/~ozoneholeandclimate/jpo-d-17-0025.1.pdf WebNov 6, 2024 · An ocean current is a continuous, directed movement of seawater generated by forces acting upon this mean flow, such as breaking waves, wind, the Coriolis effect, cabbeling, temperature and salinity differences, while tides are caused by the gravitational pull of the Sun and Moon. Depth contours, shoreline configurations, and interactions with ... WebOct 26, 2024 · Oceanic current is the continuous movement of the waters generated by a number of forces acting simultaneously upon the water, including wind, Coriolis effect, breaking waves, cabbeling, temperature, and salinity. The primary factor responsible for the movement of oceanic waters is the sea breeze and temperature. hero marketing digital