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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 18, issue 3
Ann. Geophys., 18, 347-364, 2000
https://doi.org/10.1007/s00585-000-0347-9
© European Geosciences Union 2000
Ann. Geophys., 18, 347-364, 2000
https://doi.org/10.1007/s00585-000-0347-9
© European Geosciences Union 2000

  31 Mar 2000

31 Mar 2000

Interannual signals in length of day and atmospheric angular momentum

R. Abarco del Rio1, D. Gambis2, and D. A. Salstein3 R. Abarco del Rio et al.
  • 1Spaceflight Dynamics Department, CS, 1 3 rue Villet - ZI du Palays BP 4042-31029 Toulouse Cedex 4-France
  • E-mail: Rodrigo.Abarca-del-Rio@cisi.cnes.fr
  • 2International Earth Rotation Service, (IERS), URA1125, Observatoire de Paris, 61 Av. de l'Observatoire, Paris, France
  • 3Atmospheric and Environmental Research, Inc., 840 Memorial Drive, Cambridge, MA 02139-3794, USA
  • Correspondence to: R. Abarca del Rio

Abstract. Atmospheric angular momentum (AAM) and length of day (LOD) series are investigated for their characteristics on interannual time scales during the half-century period 1949 to 1998. During this epoch, the interannual variability in LOD can be separated naturally into three bands: a quasi-biennial, a triennial-quadrennial and one at six-seven years. The atmosphere appears to excite the first two bands, while it does not contribute to the last. Considering the quasi-biennial (QB) band alone, the atmosphere appears to excite most of its signal in LOD, but it arises from separate fluctuations with stratospheric and tropospheric origin. Thus, although close in frequency, stratospheric and tropospheric processes differ in their amplitude and phase variability. The time shift can be noted especially during the strong El Niño events of 1982-83 and 1997-98 when both processes have positive phase and thus combine to help produce particularly strong peak in AAM and LOD. In addition, we have reconfirmed the downward propagation in the stratosphere and upward propagation in the troposphere of AAM observed in earlier studies for other variables. In the triennial-quadrennial (TQ) band, time-variable spectral analyses reveal that LOD and AAM contain strong variability, with periods shorter than four years before 1975 and longer thereafter. This signal originates mainly within the troposphere and propagates upwards from the lower to the higher layers of the troposphere. According to a zonal analysis, an equatorial poleward mode, strongly linked to the SOI, explains more than 60% of the total variability at these ranges. In addition, this study also indicates that an equatorward mode, originating within polar latitudes, explains, on average, more than 15% of the triennial-quadrennial oscillation (TQO) variability in AAM, and up to 30% at certain epochs. Finally, a six year period in LOD noted in earlier studies, as well as in lengthier series covering much of the century, is found to be absent in atmospheric excitations, and it is thus likely to arise from mantle/core interactions.

Key words: Meteorology and atmospheric dynamics (general circulation) - Solar physics, astrophysics and astronomy (celestial mechanics)

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