Download presentation
Presentation is loading. Please wait.
Published byFerdinand O’Neal’ Modified over 9 years ago
1
CLIVAR/GODAE Synthesis Evaluation Item#5: volume transport, temperature & salinity fluxes through key straits: Indonesian throughflow (ITF) ACC at Drake Passage Florida Current at Florida Strait Tony Lee, JPL
2
Some details about legends 3D-VAR RTS smoother
3
ITF
4
ITF volume transport (Sv) Anomaly relative to 1993-2001 mean Total Spinup problem Remarkable consistency Island Rule doesn’t work? Or effect of geometry/topography?
5
ITF volume transport from 1992 (Sv) Total Anomaly relative to 1993-2001 mean
6
ITF temperature flux (PW) Total Anomaly relative to 1993-2001 mean
7
ITF temperature flux from 1992 Total Anomaly relative to 1993-2001 mean
8
ITF salinity flux Total Anomaly relative to 1993-2002 mean
9
ITF salinity flux from 1992 Total Anomaly relative to 1993-2001 mean
10
1993-2001 averaged seasonal anomaly of ITF
11
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.
12
ACC
13
ACC volume transport Total Anomaly relative to 1993-2001 mean
14
ACC volume transport from 1992 Total Anomaly relative to 1993-2001 mean
15
ACC temperature flux Total Anomaly relative to 1993-2001 mean Relatively consistent decadal variability No such large adjustment in volume transport
16
ACC temperature flux from 1992 Total Anomaly relative to 1993-2001 mean
17
ACC salinity flux Total Anomaly relative to 1993-2001 mean
18
ACC salinity flux from 1992 Total Anomaly relative to 1993-2001 mean
19
1993-2001 averaged seasonal anomaly of ACC
20
Relatively large difference in mean and seasonal variability, but relatively consistent on decadal time scale.
21
Florida Current at Florida Strait
22
Two different ways of computing Florida Current (FC) transport by various groups: (1) meridional transport near 26.5N between Florida (~80W) to 75W (more consistent with cable measurements), (2) 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)
23
FC volume transport Anomaly relative to 1993-2001 mean Total Grey curve – cable data
24
FC volume transport from 1992 Total Anomaly relative to 1993-2001 mean Grey curve – cable data
25
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
26
FC temperature flux Total Anomaly relative to 1993-2001 mean
27
FC temperature flux from 1992 Total Anomaly relative to 1993-2001 mean
28
FC salinity flux Total Anomaly relative to 1993-2001 mean
29
FC salinity flux from 1992 Total Anomaly relative to 1993-2001 mean
30
1993-2001 averaged seasonal anomaly of Florida Current
31
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.
32
Summary Statistics
33
ITFFCACCITFtITFsFCtFCsACCtACCs Sv PW Kg/s K7-12.4157 CRFS-A-12.916.6147 CRFS-2-13.224.2147 ECCO-50yr-11.029.3129-0.42.11.11.44.5 ECCO-SIO-10.730.6154-0.9-0.42.21.11.65.3 ECMWF-10.614.8148 GFDL-15.724.3171-0.61.60.81.76.1 INGV-11.924.61272.80.9 MOVE-G-23.4179 ECCO-JPLKF-13.227.6132-1.2-0.52.31.01.44.6 MCTR 3DVAR-18.715.0142 MCTR KF-12.821.8149 ECCO-GODAE-11.126.6148-0.9-0.41.91.01.55.1 SODA-14.527.5158-1.2-0.52.11.01.75.6 Obs. Analysis-10 ~ -15 31.9120~ 160 1993-2001 mean transports/fluxes: For Florida Current: black - meridional transport near 26.5N, 80-75W; red – zonal transport between Florida & Cuba.
34
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?
35
(all in Sv)ITFFCACCrms dev. of FC from cable data K73.57.0 CRFS-A5.04.76.44.9 CRFS-25.24.76.25.3 ECCO-50yr2.41.64.12.9 ECCO-SIO.it692.52.24.63.1 ECMWF3.02.24.03.0 GFDL2.52.85.03.6 INGV3.15.63.55.5 MOVE-G4.06.3 ECCO-JPL RTS smoother 3.0 4.13.4 MCTR 3DVAR5.55.16.65.3 MCTR KF3.21.44.62.8 ECCO-GODAE.v2.1992.62.24.43.3 SODA4.32.64.55.0 rms diff. among models2.33.03.5 Measurement2.5 1993-2001 rms variability of volume transport, rms difference among models, and rms difference from cable measurements
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.