The Relationship between Sea Surface Temperature and Thermocline Depth in the Eastern Equatorial Pacific
- 1 March 2004
- journal article
- Published by American Meteorological Society in Journal of Physical Oceanography
- Vol. 34 (3) , 643-655
- https://doi.org/10.1175/2523.1
Abstract
The time dependence of the local relation between sea surface temperature (SST) and thermocline depth in the central and eastern equatorial Pacific Ocean is analyzed for the period 1990–99, using subsurface temperature measurements from the Tropical Atmosphere–Ocean Array/Triangle Trans-Ocean Buoy Network (TAO/TRITON) buoy array. Thermocline depth anomalies lead SST anomalies in time, with a longitude-dependent delay ranging from 2 weeks in the eastern Pacific to 1 year in the central Pacific. The lagged correlation between thermocline depth and SST is strong, ranging from r > 0.9 in the east to r ≈ 0.6 at 170°W. Time-lagged correlations between thermocline depth and subsurface temperature anomalies indicate vertical advection of temperature anomalies from the thermocline to the surface in the eastern Pacific. The measurements are compared with the results of forced OGCM and linear model experiments. Using model results, it is shown that the delay between thermocline depth and SST is caused mainl... Abstract The time dependence of the local relation between sea surface temperature (SST) and thermocline depth in the central and eastern equatorial Pacific Ocean is analyzed for the period 1990–99, using subsurface temperature measurements from the Tropical Atmosphere–Ocean Array/Triangle Trans-Ocean Buoy Network (TAO/TRITON) buoy array. Thermocline depth anomalies lead SST anomalies in time, with a longitude-dependent delay ranging from 2 weeks in the eastern Pacific to 1 year in the central Pacific. The lagged correlation between thermocline depth and SST is strong, ranging from r > 0.9 in the east to r ≈ 0.6 at 170°W. Time-lagged correlations between thermocline depth and subsurface temperature anomalies indicate vertical advection of temperature anomalies from the thermocline to the surface in the eastern Pacific. The measurements are compared with the results of forced OGCM and linear model experiments. Using model results, it is shown that the delay between thermocline depth and SST is caused mainl...Keywords
This publication has 28 references indexed in Scilit:
- On the Impact of Local Feedbacks in the Central Pacific on the ENSO CycleJournal of Climate, 2003
- Strong El Niño events and nonlinear dynamical heatingGeophysical Research Letters, 2003
- The Equatorial Thermocline Outcropping—A Seasonal Control on the Tropical Pacific Ocean–Atmosphere Instability StrengthJournal of Climate, 2002
- Balanced Ocean-Data Assimilation near the EquatorJournal of Physical Oceanography, 2002
- FLUID DYNAMICS OF El NIÑO VARIABILITYAnnual Review of Fluid Mechanics, 2002
- A Stability Analysis of Tropical Ocean–Atmosphere Interactions: Bridging Measurements and Theory for El NiñoJournal of Climate, 2001
- El Niño and La Niña—equatorial Pacific thermocline depth and sea surface temperature anomalies, 1986–98Geophysical Research Letters, 2001
- Thermocline and Zonal Advective Feedbacks Within the Equatorial Ocean Recharge Oscillator Model for ENSOGeophysical Research Letters, 1999
- An Equatorial Ocean Recharge Paradigm for ENSO. Part I: Conceptual ModelJournal of the Atmospheric Sciences, 1997
- Interannual Variability in a Tropical Atmosphere–Ocean Model: Influence of the Basic State, Ocean Geometry and NonlinearityJournal of the Atmospheric Sciences, 1989