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CLIVAR/GODAE Synthesis Evaluation. Tony Lee, JPL. Item#5: volume transport, temperature & salinity fluxes through key straits: Indonesian throughflow (ITF) ACC at Drake Passage Florida Current at Florida Strait. RTS smoother. 3D-VAR. Some details about legends. ITF.
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CLIVAR/GODAE Synthesis Evaluation Tony Lee, JPL • Item#5: volume transport, temperature & salinity fluxes through key straits: • Indonesian throughflow (ITF) • ACC at Drake Passage • Florida Current at Florida Strait
RTS smoother 3D-VAR Some details about legends
ITF volume transport (Sv) Total Spinup problem Island Rule doesn’t work? Or effect of geometry/topography? Anomaly relative to 1993-2001 mean Remarkable consistency
ITF volume transport from 1992 (Sv) Total Anomaly relative to 1993-2001 mean
ITF temperature flux (PW) Total Anomaly relative to 1993-2001 mean
ITF temperature flux from 1992 Total Anomaly relative to 1993-2001 mean
ITF salinity flux Total Anomaly relative to 1993-2002 mean
ITF salinity flux from 1992 Total Anomaly relative to 1993-2001 mean
ITF property flux (volume, heat, and salt) estimated by various products are overall consistent (for mean as well as for seasonal, interannual, and decadal variability: e.g., large magnitude of seasonal cycle relative to mean value, low ITF during El Nino, lack of decadal variability.
ACC volume transport Total Anomaly relative to 1993-2001 mean
ACC volume transport from 1992 Total Anomaly relative to 1993-2001 mean
ACC temperature flux Total No such large adjustment in volume transport Relatively consistent decadal variability Anomaly relative to 1993-2001 mean
ACC temperature flux from 1992 Total Anomaly relative to 1993-2001 mean
ACC salinity flux Total Anomaly relative to 1993-2001 mean
ACC salinity flux from 1992 Total Anomaly relative to 1993-2001 mean
Relatively large difference in mean and seasonal variability, but relatively consistent on decadal time scale.
Two different ways of computing Florida Current (FC) transport by various groups: • meridional transport near 26.5N between Florida (~80W) to 75W (more consistent with cable measurements), • zonal transport between Florida and Cuba (better defined in models). • The time mean of (2) is significantly smaller than that of (1) because a portion of (1) comes through a “short circuit” north of the Caribbean instead of from the loop Current (esp. in models)
FC volume transport Total Grey curve – cable data Anomaly relative to 1993-2001 mean
FC volume transport from 1992 Total Grey curve – cable data Anomaly relative to 1993-2001 mean
Zonal (upper) and meridional (lower) Florida Current transports Zonal: between Florida & Cuba (well-defined) Meridional: 26.5N, 80-75W (near cables) Grey curve – cable data
FC temperature flux Total Anomaly relative to 1993-2001 mean
FC temperature flux from 1992 Total Anomaly relative to 1993-2001 mean
FC salinity flux Total Anomaly relative to 1993-2001 mean
FC salinity flux from 1992 Total Anomaly relative to 1993-2001 mean
Relatively large spread, partly because of definition problem. In most models, the flow going into the Gulf of Mexico is weak; some flow take a short cut north of Cuba to joint the Florida Current.
1993-2001 mean transports/fluxes: For Florida Current: black - meridional transport near 26.5N, 80-75W; red – zonal transport between Florida & Cuba.
The largest mean ITF (> 23Sv): consistent with Island rule (integration of South Pacific curl)? Or effect of geometry/topography? High mean ACC transports (170-180 Sv): too strong zonal wind? lack of form drag due to smooth topography? Small viscosity?
1993-2001 rms variability of volume transport, rms difference among models, and rms difference from cable measurements