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Vertical thermohaline structure of mesoscale eddies in the four major Eastern Boundary Upwelling Systems
Cori Pegliasco1*, Alexis Chaigneau1, Rosemary Morrow1, Yves Morel 1
* Presenting author
1) Laboratoire d'Etudes en Géophysique et Océanographie Spatiales (LEGOS), France
cori.pegliasco@legos.obs-mip.fr
Introduction
Eastern Boundary Upwelling Systems (EBUS) are caracterized by:
→ Cold and productive water upwelled near the coast
CALUS
CANUS
BENUSPCUS
Introduction
Eastern Boundary Upwelling Systems (EBUS) are caracterized by:
[Colas, 2008]
x
PCUS
→ Cold and productive water upwelled near the coast→ Equatoward surface currents→ Poleward subsurface currents
CALUS
CANUS
BENUS
Introduction
Eastern Boundary Upwelling Systems (EBUS) are caracterized by:
[Colas, 2008]
x
x
[Barton, 2004]
x
x
[Veitch, 2010]
→ Cold and productive water upwelled near the coast→ Equatoward surface currents→ Poleward subsurface currents→ Strong vertical shear
CALUS
[Marchesiello, 2002]
CANUS
BENUSPCUS
Introduction
Eddy genesis
[Chaigneau et al., 2009]
Introduction
Eddy genesis
[Chaigneau et al., 2009]
Eddy propagation velocity
Introduction
Eddy genesis
[Chaigneau et al., 2009]
Eddy propagation velocity
Do eddies also share similar vertical structure ?
Objective
Depict the eddy vertical structure in the 4 EBUS,combining altimetry and ARGO floats profiles
Objective
Depict the eddy vertical structure in the 4 EBUS,combining altimetry and ARGO floats profiles
[Yu et al., 2012]
CEs AEs
[Chaigneau et al., 2011] θ' (°C)
[Yang et al., 2013]
North-West Pacific North-West Pacific South-East Pacific
Data & Method
Weekly altimetry maps
2001 - 2012
Automated eddy detection skills (amplitude > 2 cm)[Chaigneau et al., 2008]
PCUS
Data & Method
PCUSARGO profiles
+altimetry
Classification of the ARGO profiles within CE, AE or outside eddies
4 CEs4 AEs14 Out
Profiles :
Data & Method
Outside Eddies (OEs) ~60 %
4450
8000
9800
8700
2100
3000
26001300
2900
2300
13002300
Cyclonic Eddies (CEs) ~20 %
Anticyclonic Eddies (AEs) ~20 %
Data & Method
Outside Eddies (OEs) ~60 %
4450
8000
9800
8700
2100
3000
26001300
2900
2300
13002300
Cyclonic Eddies (CEs) ~20 %
Anticyclonic Eddies (AEs) ~20 %
→ Temperature and salinity anomalies
Data & Method
< 200 km+/- 1 month
→ local mean
PCUS
Data & Method
Done for all the availables profiles→ within AEs→ within CEs
→ outside eddies
PCUS
Results : Mean temperature anomaly
AEs
CEs
OEs
Results : Mean temperature anomaly
AEs
CEs
OEs
Results : Mean temperature anomaly
T' : -150m-0,45 °C T' : -330m
0,3°C
Results : Mean temperature anomaly
T' : -120m-0,6 °C
T' : -170m 0,5°C
Results : Mean temperature anomaly
T1' : -80m
-0,5 °C
T1' : -70m
0,5°C
Results : Mean temperature anomaly
T1' : -80m
-0,5 °C
T1' : -70m
0,5°C
T2' : -1360m
0,1°C T
2' : -1460m
0,1°C
Results : Mean temperature anomaly
T1' : -160m
-0,4 °CT
1' : -230m
0,5°C
Results : Mean temperature anomaly
T1' : -160m
-0,4 °CT
1' : -230m
0,5°C
T2' : -470m
-0,4 °CT
2' : -500m
0,5°C
Results : Mean temperature anomaly
Enough Argo profiles to look more in details
Results : Mean temperature anomaly in subregions (CANUS)
CANUS
Mean anomaly
Results : Mean temperature anomaly in subregions (CANUS)
CANUS
Mean anomaly
[Barton, 2004]
Cape Verde Frontal Zone
Results : Mean temperature anomaly in subregions (CANUS)
CANUS
Mean anomaly
Cape Verde Frontal Zone
Meddies influence
[Richardson, 1998]
Temperature within a Meddy[Richardson, 2000]
« Meddy » profile
Results : Mean temperature anomaly in subregions (BENUS)
BENUS
Mean anomaly
Results : Mean temperature anomaly in subregions (BENUS)
BENUS
Mean anomaly
Few eddies + few profiles
Profiles withinCEs
Profiles withinAEs
Results : Mean temperature anomaly in subregions (BENUS)
BENUS
Mean anomaly
[Veitch, 2010]
[Matano, 2003]
Conclusions
● Altimetry + Argo floats profiles → efficient tool to reconstruct the eddy vertical structure
+ =
CALUS
Conclusions
● Altimetry + Argo floats profiles→ efficient tool to reconstruct the eddy vertical structure
● Strong differences between each EBUS
PCUS CALUS BENUS CANUS
+ =
CALUS
Conclusions
● Altimetry + Argo floats profiles→ efficient tool to reconstruct the eddy vertical structure
● Strong differences between each EBUS
● Strong heterogeneity within each EBUS
PCUS CALUS BENUS CANUS
North
South
+ =
CALUS
Perspectives
● Work on salinity anomalies
T' S' T' S'
PCUS CANUS
Perspectives
● Work on salinity anomalies
● Track eddies in time and space to depict the evolution of their vertical structure
T' S' T' S'
PCUS CANUS
[Sangra, 2009]
Perspectives
● Work on salinity anomalies
● Track eddies in time and space to depict the evolution of their vertical structure
● Separate the different kinds of eddies
T' S'
→ « Meddy » profile
→ « North » profile
→ « South » profile
T' S'
PCUS CANUS
[Sangra, 2009]
AEs
Perspectives
● Work on salinity anomalies
● Track eddies in time and space to depict the evolution of their vertical structure
● Separate the different kinds of eddies
● Find the dynamicals mecanisms leading to such different structures
T' S'
→ « Meddy » profile
→ « North » profile
→ « South » profile
T' S'
PCUS CANUS
[Sangra, 2009]
AEs
Mean Temperature anomaly
Mean Salinity anomaly
PCUS Subregions : Salinity anomaly
CALUS Subregions : Salinity anomaly
CANUS Subregions : Salinity anomaly
BENUS Subregions : Salinity anomaly
PCUS Subregions : Temperature anomaly
PCUS
Mean anomaly
Mean anomaly
[Parada et al., 2012]
PCUS Subregions : Temperature anomaly
CALUS
Mean anomaly
CALUS Subregions : Temperature anomaly
CALUS
Mean anomaly
[Strub and James, 2002]
CALUS Subregions : Temperature anomaly
Clustering : « water classes »
● Cluster analysis (comparing similarities)
→ Consistent with the local circulation
→ Between T and S profiles :
Clustering : AEs of CANUS
● Cluster analysis (comparing similarities)
→ Between T and S anomalies profiles within AEs→ Between T and S profiles
→ « Meddy » profile
→ « North » profile
→ « South » profile
● Cluster analysis (comparing similarities)
→ Between T and S anomalies profiles within AEs→ Between T and S anomalies profiles within CEs
→ Between T and S profiles
→ « Meddy ? » profile
→ « North » profile
→ « South » profile
Clustering : CEs of CANUS
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