Relationship between El Niño–Southern Oscillation and the Symmetry of the Hadley Circulation: Role of the Sea Surface Temperature Annual Cycle

El Niño–Southern Oscillation (ENSO), which features an equatorial quasi-symmetric sea surface temperature anomaly (SSTA), is related to both the symmetric and asymmetric components of the Hadley circulation (HC) variability. However, the mechanisms for such a nonlinear HC–ENSO relationship are still...

Full description

Saved in:
Bibliographic Details
Published in:Journal of climate 2018-07, Vol.31 (13), p.5319-5332
Main Authors: Guo, Yi-Peng, Tan, Zhe-Min
Format: Article
Language:English
Subjects:
Annual variations
Asymmetry
Atmospheric sciences
Convection
El Nino
El Nino effects
El Nino phenomena
El Nino-Southern Oscillation event
Equator
Hadley circulation
Hurricanes
Impact prediction
La Nina
La Nina events
Laboratories
Oscillators
Sea surface
Sea surface temperature
Sea surface temperature anomalies
Southern Oscillation
Summer
Surface temperature
Symmetry
Temperature
Temperature anomalies
Variability
Wind
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:El Niño–Southern Oscillation (ENSO), which features an equatorial quasi-symmetric sea surface temperature anomaly (SSTA), is related to both the symmetric and asymmetric components of the Hadley circulation (HC) variability. However, the mechanisms for such a nonlinear HC–ENSO relationship are still unclear. Using 36-yr monthly reanalysis datasets, this study shows that the month-to-month HC variability is dominated by two principal modes, the asymmetric mode (AM) and symmetric mode (SM), both of which are highly correlated with ENSO variability. Furthermore, the relationship between the HC principal modes and the ENSO SSTA is modulated by the western Pacific SST annual cycle. When the zonal mean western Pacific SST peaks off (on) the equator, the ENSO SSTA leads to the AM (SM) of HC variability. This is because the zonal mean western Pacific SST peak provides a warmer background favorable for the SSTA to stimulate convection, indicating the important role of the combined effect of the SST annual cycle and the ENSO SSTA in affecting the HC variability. Importantly, the western Pacific SST annual cycle has no such modulation effect during central Pacific El Niño or La Niña events. The results have important implications for simulating and predicting the climatic impacts of ENSO and HC variability.
ISSN:0894-8755
1520-0442
DOI:10.1175/JCLI-D-17-0788.1