Not exact matches
The green
layer is the lithospheric plate, which forms at the mid
ocean ridge, then cools down and
thickness as it moves away from the ridge.
Drushka, K., J. Sprintall, and S. T. Gille, 2014: Subseasonal variations in salinity and barrier -
layer thickness in the eastern equatorial Indian
Ocean, J. Geophys.
The close relationship that exists between the dynamic height and the mass field of the
ocean allows these two parameters to be used within a two -
layer reduced gravity
ocean model to monitor the upper
layer thickness (Goni et al., 1996), which is defined in this study to go from the sea surface to the depth of the 20 °C isotherm.