Seasonal and interannual variations of the energy flux equator and ITCZ. Part I: Zonally averaged ITCZ position

Ori Adam*, Tobias Bischoff, Tapio Schneider

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

109 Scopus citations

Abstract

In the zonal mean, the ITCZ lies at the foot of the ascending branch of the tropical mean meridional circulation, close to where the near-surface meridional mass flux vanishes. The ITCZ also lies near the energy flux equator (EFE), where the column-integrated meridional energy flux vanishes. This latter observation makes it possible to relate the ITCZ position to the energy balance, specifically the atmospheric net energy input near the equator and the cross-equatorial energy flux. Here the validity of the resulting relations between the ITCZ position and energetic quantities is examined with reanalysis data for the years 1979-2014. In the reanalysis data, the EFE and ITCZ position indeed covary on time scales of seasons and longer. Consistent with theory, the ITCZ position is proportional to the cross-equatorial atmospheric energy flux and inversely proportional to atmospheric net energy input at the equator. Variations of the cross-equatorial energy flux dominate seasonal variations of the ITCZ position. By contrast, variations of the equatorial net energy input, driven by ocean energy uptake variations, dominate interannual variations of the ITCZ position (e.g., those associated with ENSO).

Original languageAmerican English
Pages (from-to)3219-3230
Number of pages12
JournalJournal of Climate
Volume29
Issue number9
DOIs
StatePublished - 1 May 2016
Externally publishedYes

Bibliographical note

Publisher Copyright:
© 2016 American Meteorological Society.

Keywords

  • Atmospheric circulation
  • Circulation/dynamics
  • Climate variability
  • Energy budget/balance
  • Interannual variability
  • Physical meteorology and climatology
  • Tropical variability
  • Variability

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