In this study, a reduced-rank stationary Kalman filter is used to assimilate TOPEX/Poseidon sea-s... more In this study, a reduced-rank stationary Kalman filter is used to assimilate TOPEX/Poseidon sea-surface height anomaly (SHA) data into a realistic model of the tropical Atlantic Ocean. The goal is to assess how the interhemispheric transports between the Atlantic subtropics and tropics are affected by the assimilation of TOPEX/Poseidon altimetry and how the subsurface thermocline structure is dynamically constrained by
... In the ocean GCM, the deep mixed layer occurs in the northern part of subtropical gyre and sh... more ... In the ocean GCM, the deep mixed layer occurs in the northern part of subtropical gyre and shoals abruptly in the central ... and advected southwestward, the low potential vorticity fluid in each isopycnal overlaps that on another isopycnal and makes a thick low potential vorticity ...
In this study, a reduced-rank stationary Kalman filter is used to assimilate TOPEX/Poseidon sea-s... more In this study, a reduced-rank stationary Kalman filter is used to assimilate TOPEX/Poseidon sea-surface height anomaly (SHA) data into a realistic model of the tropical Atlantic Ocean. The goal is to assess how the interhemispheric transports between the Atlantic subtropics and tropics are affected by the assimilation of TOPEX/Poseidon altimetry and how the subsurface thermocline structure is dynamically constrained by
... In the ocean GCM, the deep mixed layer occurs in the northern part of subtropical gyre and sh... more ... In the ocean GCM, the deep mixed layer occurs in the northern part of subtropical gyre and shoals abruptly in the central ... and advected southwestward, the low potential vorticity fluid in each isopycnal overlaps that on another isopycnal and makes a thick low potential vorticity ...
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