FastFind »   Lastname: doi:10.1029/ Year: Advanced Search  

AGU: Geophysical Research Letters

 

Keywords

  • antarctic circumpolar current
  • length of day
  • ocean angular momentum

Index Terms

  • 1239 - Earth rotation variations
  • 1622 - Earth system modeling
  • 3339 - Ocean/atmosphere interactions
  • 4512 - Currents
  • 4550 - Ocean influence of Earth rotation

Paper in Press

GEOPHYSICAL RESEARCH LETTERS, doi:10.1029/2011GL050671

Detection of the Earth rotation response to a rapid fluctuation of Southern Ocean circulation in November 2009

Key Points
  • A rapid drop and recovery in the Antarctic Circumpolar Current occurred in 2009
  • The resulting anomaly in oceanic angular momentum changed the length of day.
  • This unique LOD signature highlights the unusual Southern Ocean state in 2009

Authors:

Steven L. Marcus

Jean O. Dickey

Ichiro Fukumori

Olivier de Viron

At seasonal and shorter periods the solid Earth and its overlying geophysical fluids form a closed dynamical system, which (except for tidal forcing) conserves its total angular momentum. While atmospheric effects dominate changes in the Earth's rate of rotation and hence length-of-day (LOD) on these time scales, the addition of oceanic angular momentum (OAM) estimates has been shown to improve closure of the LOD budget in a statistical sense. Here we demonstrate, for the first time, the signature of a specific, sub-monthly ocean current fluctuation on the Earth's rotation rate, coinciding with recently-reported anomalies which developed in southeast Pacific surface temperature and bottom pressure fields during late 2009. Our results show that concurrent variations in the Antarctic Circumpolar Current (ACC), which saw a sharp drop and recovery in zonal transport during a two-week period in November, were strong enough to cause a detectable change in LOD following the removal of atmospheric angular momentum (AAM) computed from the Modern Era Retrospective Analysis for Research and Applications (MERRA) database. The strong OAM variations driving the LOD-AAM changes were diagnosed from ocean state estimates of the Consortium for Estimating the Circulation and Climate of the Ocean (ECCO) and involved roughly equal contributions from the current and pressure terms, with in situ confirmation for the latter provided by tide-corrected bottom pressure recorder data from the South Drake Passage site of the Antarctic Circumpolar Current Levels by Altimetry and Island Measurements (ACCLAIM) network.

Received 15 December 2011; accepted 30 January 2012.

Citation: Marcus, S. L., J. O. Dickey, I. Fukumori, and O. de Viron (2012), Detection of the Earth rotation response to a rapid fluctuation of Southern Ocean circulation in November 2009, Geophys. Res. Lett., doi:10.1029/2011GL050671, in press.