ENSO modulation of tropical Indian Ocean subseasonal variability

Abstract

In this study, we use 30 years of retrospective climate model forecasts and observational estimates to show that El Niño/Southern Oscillation (ENSO) affects the amplitude of subseasonal variability of sea surface temperature (SST) in the southwest Indian Ocean, an important Tropical Intraseasonal Oscillation (TISO) onset region. The analysis shows that deeper background mixed‐layer depths and warmer upper ocean conditions during El Niño reduce the amplitude of the subseasonal SST variability over Seychelles‐Chagos Thermocline Ridge (SCTR), which may reduce SST‐wind coupling and the amplitude of TISO variability. The opposite holds for La Niña where the shallower mixed‐layer depth enhances SST variability over SCTR, which may increase SST‐wind coupling and the amplitude of TISO variability.

Document Details

Document Type
Pub Defense Publication
Publication Date
Dec 28, 2016
Source ID
10.1002/2016gl071899

Entities

People

  • Ben Kirtman
  • Eunsil Jung

Organizations

  • National Institute of Meteorological Sciences
  • National Oceanic and Atmospheric Administration
  • Office of Naval Research
  • University of Miami

Tags

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Atmospheric Science/Meteorology
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers