Phase Synchronization of the El Niño-Southern Oscillation with the Annual Cycle

Karl Stein, Axel Timmermann, and Niklas Schneider
Phys. Rev. Lett. 107, 128501 – Published 13 September 2011

Abstract

The El Niño-Southern Oscillation (ENSO) is the largest global climate signal on the interannual time scale. ENSO events occur irregularly, yet individual events follow a similar pattern of developing during boreal summer or fall and peaking during boreal winter. This characteristic of ENSO is often referred to as “phase locking” of ENSO with the annual cycle. However, no observational evidence of phase interaction between the two phenomena has thus far been presented. In this study, we analyze sea surface temperature observations and find the first evidence of partial phase synchronization of ENSO with the annual cycle.

  • Figure
  • Figure
  • Figure
  • Received 17 April 2011

DOI:https://doi.org/10.1103/PhysRevLett.107.128501

© 2011 American Physical Society

Authors & Affiliations

Karl Stein

  • Department of Oceanography, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, Hawaii 96822, USA

Axel Timmermann and Niklas Schneider

  • International Pacific Research Center & Department of Oceanography, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, Hawaii 96822, USA

Article Text (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 107, Iss. 12 — 16 September 2011

Reuse & Permissions
Access Options
CHORUS

Article Available via CHORUS

Download Accepted Manuscript
Author publication services for translation and copyediting assistance advertisement

Authorization Required


×
×

Images

×

Sign up to receive regular email alerts from Physical Review Letters

Log In

Cancel
×

Search


Article Lookup

Paste a citation or DOI

Enter a citation
×