Robertson, J.D., C.R. Bentley, J.W. Clough, and L.L. Greischar,
Sea bottom topography and crustal structure below the Ross Ice Shelf, Antarctica, in Antarctic Geoscience (C. Craddock, ed.)
Not exact matches
And scientists now know that the underwater
topography — the hills, slopes and crevices at the
bottom of the ocean, where the ice meets the
sea — is a critical influence on just how much ice actually touches the water.
Also, you can start by exploring an illustrated view of the array of factors — from
sea -
bottom topography to warm water — that may be in play in the changing Arctic Ocean provided by James Morison of the University of Washington.
Local
topography, bay and river orientation, depth of the
sea bottom, astronomical tides, as well as other physical features, are taken into account in a predefined grid referred to as a SLOSH basin.
He has done extensive work on modeling and interpretation of
sea level and ocean
bottom pressure signals and is currently a member of various NASA satellite mission science teams (Ocean Surface
Topography, GRACE, Ocean Surface Salinity) and the GODAE OceanView Science Team.
Features of the model described here include the following: (1) tripolar grid to resolve the Arctic Ocean without polar filtering, (2) partial
bottom step representation of
topography to better represent topographically influenced advective and wave processes, (3) more accurate equation of state, (4) three - dimensional flux limited tracer advection to reduce overshoots and undershoots, (5) incorporation of regional climatological variability in shortwave penetration, (6) neutral physics parameterization for representation of the pathways of tracer transport, (7) staggered time stepping for tracer conservation and numerical efficiency, (8) anisotropic horizontal viscosities for representation of equatorial currents, (9) parameterization of exchange with marginal
seas, (10) incorporation of a free surface that accommodates a dynamic ice model and wave propagation, (11) transport of water across the ocean free surface to eliminate unphysical «virtual tracer flux» methods, (12) parameterization of tidal mixing on continental shelves.