interannual variability of the tropical-subtropical connections in the atlantic
DESCRIPTION
Interannual variability of the tropical-subtropical connections in the Atlantic. Sabine Hüttl, IFM-GEOMAR Kiel. Outline. mean state at 35°W , EUC, NBC interannual variability in the STC-regime what spatial patterns ? what amplitudes & timescales ? what mechanisms ? - PowerPoint PPT PresentationTRANSCRIPT
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Interannual variability of the tropical-subtropical connections in the
Atlantic
Sabine Hüttl, IFM-GEOMAR Kiel
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• mean state at 35°W, EUC, NBC
• interannual variability in the STC-regime
• what spatial patterns ?• what amplitudes & timescales ?• what mechanisms ?
• changes in the strength of the STC (v‘T)• changes by advection of temperature anomalies (v T')
• role of NEUC/SEUC for the supply of the off-equatorial upwelling regions
Outline
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Models & configurations
FLAME-model configurations:
• 1/3° Atlantic:
• forcing: NCEP 1958-1999
- HEAT only
- HEAT+WIND
• 1/12° North Atlantic
• climatological ECMWF forcing
• both: 45 z-level, rigid-lid, BBL, iso-
pycnal mixing, GM90
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Mean zonal circulation at 35°W
observational mean 1/3° november mean 1/12° november mean (Schott et al., 2003)
EUC
SEUC
SICC
EIC
NICC
NBC
SEC SEC
NEUCNBC
SEC
EUC
SEUC NEUC
SEC
EUCNBC
SEUCNEUC
SEC SEC
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Mean zonal circulation at 35°W
EUC
SEUC
SICC
EIC
NICC
NBC
SEC SEC
NEUCNBC
SEC
EUC
SEUC NEUC
SEC
EUCNBC
SEUCNEUC
SEC SEC
observational mean 1/3° mean 1/12° mean (Schott et al., 2003)
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Mean zonal circulation at 35°W
EUC: max. 75 cm/s, 20.9 SvNBC: max. 60 cm/s, -32.2 Sv EIC: 10.2 Sv NEUC, SEUC > 10 cm/s
max. 60 cm/s, 15.7 Sv max. >60 cm/s, -27.4 Sv no EIC weak mean SEUC NEUC reaches surface
max. 80 cm/s, 15.9 Sv max. >60 cm/s, -27.2 Sv no EIC weak mean SEUC NEUC 0m to 700m
1/3° 1/12°obs.
EUC
SEUC
SICC
EIC
NICC
NBC
SEC SEC
NEUCNBC
SEC
EUC
SEUC NEUC
SEC
EUCNBC
SEUCNEUC
SEC SEC
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Mean zonal circulation at 35°W
• complex structure of zonal currents is already resolved in the 1/3° (isopycnic) model, higher resolution (1/12°) gives a sharper horizontal structure, but in the mean no currents like the EIC, NICC, SICC
1/3° 1/12°obs.
EUC
SEUC
SICC
EIC
NICC
NBC
SEC SEC
NEUCNBC
SEC
EUC
SEUC NEUC
SEC
EUCNBC
SEUCNEUC
SEC SEC
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EUC variability
mean EUC at 0°N
26.2
24.4
26.025.5 • EUC bounded by the isopycnals = 24.4-26.2
• upwelling of this isopyc- nals into the mixed- layer eastward of 30°W
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EUC variability
mean EUC at 0°N
HEATHEAT+WIND
26.2
24.4
26.025.5
Interannual variability of the EUC at 35°W
• EUC bounded by the isopycnals = 24.4-26.2
• upwelling of this isopyc- nals into the mixed- layer eastward of 30°W
HEAT+WINDHEAT• nearly no variability in HEAT
(RMS <0.5 Sv)
• wind variability creates ampli- tudes up to 2 Sv
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NBC variability
mean NBC at 5°S
24.426..2
• NBC-core in the den- sity range of EUC
• northward transport of 24.3 Sv, in the STC 8.5 Sv
• broad southward recirculation (3.6 Sv) of the NBC with core near 200m
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NBC variability
mean NBC at 5°S
Interannual variability of the NBC at 5°S
24.426..2
• NBC-core in the den- sity range of EUC
• northward transport of 24.3 Sv, in the STC 8.5 Sv
• broad southward recirculation (3.6 Sv) of the NBC with core near 200m
• low variability in HEAT, high in HEAT+WIND
• phase-shift: high NBC- transport from 1960-70, low from 1970-90, high from 1991 in both expe- riments
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...bringing it together...
interannual variability of the STC
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Mean meridional overturning
... on z-levels
... on -levels
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Mean meridional overturning
... on z-levels
... on -levels
• deep MOC of >15 Sv• southern STC (~3 Sv) & TC (~2 Sv), • northern TC (~11 Sv)• equatorial upwelling: 16 Sv• most of upwelling associated with TCs
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Mean meridional overturning
... on z-levels
... on -levels
• deep MOC of >15 Sv• southern STC (~3 Sv) & TC (~2 Sv), • northern TC (~11 Sv)• equatorial upwelling: 16 Sv• most of upwelling associated with TCs
• transports in density classes are lower because of isopycnal recirculation in the TCs (Kröger, 2001)• in the EUC-density range nearly no supply of northern hemispheric water
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Mechanisms
• examination of STC transport: layer between =24.4 and 26.2 kg/m^3
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Mechanisms
• examination of STC transport: layer between =24.4 and 26.2 kg/m^3
• causes of interannual variability ?
• variations in the strength of the STC (v‘T) may caused by:
• changes in equatorial divergence ("pull")• changes in volume of subducted water ("push")
• advection of temperature anomalies from the subtropics (v T')
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Mechanisms
• examination of STC transport: layer between =24.4 and 26.2 kg/m^3
• causes of interannual variability ?
• variations in the strength of the STC (v‘T) may caused by:
• changes in equatorial divergence ("pull")• changes in volume of subducted water ("push")
• advection of temperature anomalies from the subtropics (v T')
• questions:
• concentrated at the boundary ?• meridional coherence ?• signal propagating speeds ?
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changes in the strength of STC
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• highest variability in both experiments concentrated at the western boundary• variability intensity increases about 10 times if interannual winds are used• wind variations create small fluctuations in the interior which are in the order of heat flux- driven variations in the boundary current• in HEAT+WIND signal of NBC retroflection
Variability: where ?
RMS of transport density changes in the STC density range
HEAT HEAT+WIND
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v‘T: meridional coherence ?
HEATHEAT+WIND
• amplitudes ~1 Sv• anomalies meridional coherent to 4°S• signal needs < 1 year from ~16°S to 4°S• decadal variation of NBC-transports• NBC and EUC-anomalies normally not in phase for regions south of 4°S
Interannual variability of the EUC (upper) at35°W and the NBC (lower) in Sv
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v‘T: meridional coherence ?
HEATHEAT+WIND
HEAT+WINDHEAT
• amplitudes ~1 Sv• anomalies meridional coherent to 4°S• signal needs < 1 year from ~16°S to 4°S• decadal variation of NBC-transports• NBC and EUC-anomalies normally not in phase for regions south of 4°S
Interannual variability of the EUC (upper) at35°W and the NBC (lower) in Sv
Correlation of EUC and NBC anomalies
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v‘T: meridional coherence ?
HEATHEAT+WIND
HEAT+WINDHEAT
• amplitudes ~1 Sv• anomalies meridional coherent to 4°S• signal needs < 1 year from ~16°S to 4°S• decadal variation of NBC-transports• NBC and EUC-anomalies normally not in phase for regions south of 4°S
interannual wind variability masks clear signal propagation from the subtropics to the tropics
• HEAT: meridional coherence to 0°S• variability up to 0.4 Sv• high correlations from ~12°S between EUC and NBC variability
however:
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causes of v‘T-signal ?
correlation of x in ATL3 and v‘ in NBC
correlation of x in ATL3 and v‘
• high values (0.6) in the NBC south of 4°S
• high values in all latitudes south of 4°S• correlation breaks down in the region of the southern TC
• strength of TC is highly correlated with x between 0°S and 4°S (not shown)
ATL3
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causes of v‘T-signal ?
possible explanation:
• stronger easterlies at ATL3 force stronger upwelling at the equator
• stronger upwelling needs more inflow from the south via NBC
• the stronger NBC strengthens the TC (and more north the NBC-retroflection), i.e. a stronger south- ward component near the boundary develops (corr. not shown)
• the TCs decouple the equatorial circulation changes from the changes more south
correlation of x in ATL3 and v‘
correlation of x in ATL3 and v‘ in WBC
ATL3
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Anomaly propagation
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Anomalies from the south: v T'
propagating temperature anomalies on the isopycnal 25.2 kg/m^3
• model reveals clear anomalies that propagate to the western boundary and after that north- ward
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propagating temperature anomalies on the isopycnal 25.2 kg/m^3
• strongest anomalies between 16°S & 12°S (0.6°C)
• “mean“ signals are 0.3°C, same magni- tude as RMS of inter- annual SST variability !
• most anomalies fade away on the way to the equator
• propagation in the NBC needs ~2 years
• some anomalies are visible in the EUC: 1964-65, 1968-80, 1993-94
Anomalies from the south: v T'
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Conclusions STC variability
• 1/3°-model shows a detailed equatorial zonal current system• equatorial upwelling of 16 Sv• southern STC-transport: 3 Sv (without TC !), no mean northern STC• strong TCs between 4°S/N and equator
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Conclusions STC variability
• 1/3°-model shows a detailed equatorial zonal current system• equatorial upwelling of 16 Sv• southern STC-transport: 3 Sv (without TC !), no mean northern STC• strong TCs between 4°S/N and equator
• interannual variability strongest at the boundary and weak in the interior
• transport anomalies coherent south of 4°S• decadal fluctuation of the NBC-transports• no simple connection between transport anomalies in the NBC and the EUC
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Conclusions STC variability
• 1/3°-model shows a detailed equatorial zonal current system• equatorial upwelling of 16 Sv• southern STC-transport: 3 Sv (without TC !), no mean northern STC• strong TCs between 4°S/N and equator
• interannual variability strongest at the boundary and weak in the interior
• transport anomalies coherent south of 4°S• decadal fluctuation of the NBC-transports• no simple connection between transport anomalies in the NBC and the EUC
• possible reason: wind stress variability changes the (eq.) upwelling, because of continuity this causes transport changes in the NBC (visible to 12°S), a fluctuating NBC results in fluctuating TCs
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Conclusions STC variability
• 1/3°-model shows a detailed equatorial zonal current system• equatorial upwelling of 16 Sv• southern STC-transport: 3 Sv (without TC !), no mean northern STC• strong TCs between 4°S/N and equator
• interannual variability strongest at the boundary and weak in the interior
• transport anomalies coherent south of 4°S• decadal fluctuation of the NBC-transports• no simple connection between transport anomalies in the NBC and the EUC
• possible reason: wind stress variability changes the (eq.) upwelling, because of continuity this causes transport changes in the NBC (visible to 12°S), a fluctuating NBC results in fluctuating TCs
• propagating temperature anomalies are o(0.3°C) and often do not reach the equatorial upwelling-zone, varying TC-transports blur the anomaly signals
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Work in progress
known: sources of equatorial upwelling: mainly NBC, small parts from NEC, unknown: sources of off-equatorial upwelling in the Guinea and Angola Domes
• Lagrangian analysis in 1/3° and 1/12° model with daily/monthly/annual snapshots:
Pathways of synthetic floats launched in the EUC of the 1/12° model at 20°W in May,backward in time integration after 1 year
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Work in progress
1/3° annual mean
Guinea Dome
In this mean picture:
• northern STC reaches to the NECC/NEUC-system which feeds the Guinea Dome
• only few floats came from the south
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Work in progress
1/3° annual mean
1/12° monthly mean, launch: may
Guinea Dome
Guinea Dome
In this mean picture:
• northern STC reaches to the NECC/NEUC-system which feeds the Guinea Dome
• only few floats came from the south
BUT with monthly mean forcing:
• no inflow from northern hemisphere
• nearly all water originates from the tropical regions and from the NBC !
• WHY ???
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The END
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Not shown correlations
Correlation of the NBC-variability (STC-part) withthe changes of TC-Index