Interannual signals in length of day and atmospheric angular momentum
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 triennialquadrennial and one at six-seven years. The atmosphere appears to excite the ®rst two bands, while it does not contribute to the last. Considering the quasi-biennial (QB) band alone, the
... band alone, the atmosphere appears to excite most of its signal in LOD, but it arises from separatē uctuations with stratospheric and tropospheric origin. Thus, although close in frequency, stratospheric and tropospheric processes dier in their amplitude and phase variability. The time shift can be noted especially during the strong El NinÄ o 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 recon®rmed the downward propagation in the stratosphere and upward propagation in the troposphere of AAM observed in earlier studies for other variables. In the triennialquadrennial (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.