low frequency variability of the ccs: effect of the 1997-98 el nino. x. capet, j mcwilliams, a....

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Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

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Page 1: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Low frequency variability of the CCS: effect of the 1997-98 El Nino.

X. Capet, J McWilliams, A. Shchepetkin (UCLA)

Eastern Pacific Ocean Conference 2004

Page 2: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Modeling strategy.

½ degree ROMS Pacific between 1970 and 1999. NCEP monthly forcings.

15km ROMS USWC between 1990 and 1999. Adjusted NCEP monthly forcings.

Offline coupling. Boundary

conditions updated every 10 days.

Page 3: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Pacific solution

TOPEX SSH anomaly 11/97-2/98 ROMS Pacific (0.5° grid)

Page 4: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

ENSO simulations (0.5 degrees horizontal resolution)

Sea Surface Elevation between 1995 and 1999.

Page 5: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Boundary conditions between Sep.97 and Apr. 98 (SST and v anomalies).

Sep. Oct. Nov. Dec.Sep. Jan. Feb. Mar.

Page 6: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Wind climatology.

NCEPQuikSCAT

Page 7: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Wind climatology. Temperature along CalCOFI line 67

winter spring summer fall

Page 8: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Wind variability : longshore wind stress over the nearshore region

exp0>exp1

Page 9: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Experiment exp0: full variability

SSH anomaly exp0

Pt. Conception

C. Mendocino

Page 10: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

May 97

Sep 97

Oct 97

Nov 97

Dec 97

Jan 98

Feb 98

Mar98

Apr 98

Jun 97

Temperature anomaly exp0

Page 11: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Wind Sensitivity: role of wind anomalies during El Nino 97-98.

Differences are minor everywhere expect

north of 40N at the onset and retreat of El

Nino conditions.

SSH anomaly exp0 SSH anomaly exp1

Page 12: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Temperature anomalies along the USWCOct 97

Nov 97

Dec 97

Jan 98

Page 13: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Feb 98

Mar98

Apr 98

Jun 97

Page 14: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

1- The wind anomaly has a minor influence in the onset and further development of the model 97-98 ElNino

2- The most noticeable influence of wind anomaly is north of 40°N.

3- The ocean temperature signal seems to respond to wind changes rather than absolute values.

Wind Sensitivity: role of wind anomalies during the 97-98 El Nino

Page 15: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Origin of temperature anomalies and water displacement associated with the model 97-98 ElNino signal

Nov 97 Dec 97

Spiciness at 50 m depth

Page 16: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Jan 98 Feb 98

Page 17: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Spiciness at 70 m depth Jan 98

Page 18: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Lagrangian Trajectories

3D trajectories of floats released at 50m depth 30 km offshore between 30 and 42 degrees in mid october 1997

1996

Page 19: Low frequency variability of the CCS: effect of the 1997-98 El Nino. X. Capet, J McWilliams, A. Shchepetkin (UCLA) Eastern Pacific Ocean Conference 2004

Lagrangian Trajectories

Latitude as a function of time (oct 15 to dec15) for the floats released at 50m depth