Open AccessCombining altimetry with a thermocline model to examine the transport of the North Atlantic
Author(s) -
Williams Richard G.,
Pennington Matthew
Publication year - 1999
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/1999jc900125
Subject(s) - thermocline , ocean gyre , geostrophic wind , stratification (seeds) , potential vorticity , altimeter , mixed layer , geostrophic current , oceanography , geology , climatology , sea surface height , ekman transport , subtropics , wind stress , vorticity , sea surface temperature , meteorology , geography , vortex , geodesy , upwelling , seed dormancy , botany , germination , dormancy , fishery , biology
The relationship between sea surface height and transport is explored using a steady, geostrophic, thermocline model. Given an imposed sea surface height (SSH), analytical solutions reveal different patterns for the transport over the interior of a subtropical gyre determined by the background stratification. For no mixed layer or the limit of weak stratification, transport increases more rapidly westward than SSH across a subtropical gyre, whereas in the limit of strong stratification, transport increases linearly with SSH, and streamlines become more orientated from the northwest to southeast. A modified version of the thermocline model is applied to the subtropical gyre of the North Atlantic and uses SSH from TOPEX/Poseidon altimetry and a functional relationship between potential vorticity and density derived from the National Oceanographic Data Center climatology. The model suggests that the transport over the interior of the subtropical gyre reaches 30±13 Sv, which is broadly in accord with the independent Sverdrup estimate from the wind‐stress climatology. The transport pattern includes a north‐south asymmetry, which is consistent with both the mixed layer and background stratification influencing the solution.