This shows upward fluxes through the top
of the pycnocline of about 1 watt in the Beayfort Sea, and 2 - 3 watts over the Chukchi Shelf, an area influenced by the Pacific inflow.
Not exact matches
Predicting sea ice extent is easy if you can mentally calculate wind variations, momentum, sea currents, multi year ice compression ratios, tidal synergy with weather patterns, the AO, the temperature
of ice sea water and air, how cloudy it will be, salinity,
pycnocline convection rates, sea surface to air interface, CO2 exchange, ice thickness distributions.....
«The
pycnocline (meaning rapid change
of density) separates the surface layer
of the ocean from the deep ocean.
[5] These variations
of salinity and temperature with depth change the density
of the seawater, creating the
pycnocline.
Capotondi A. (January 2008): Can the mean structure
of the tropical
pycnocline affect ENSO period in coupled climate models?
Low frequency
pycnocline depth variability at Station P in the northeast Pacific, Journal
of Physical Oceanography, 32, 3207 - 3215.