Joachim Höpfner

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At interannual time scales, the excitation of variations in Length-Of-Day (LOD) is caused by two prominent signals in the atmosphere: The El Niño-Southern Oscillation (ENSO) and the Quasi-Biennial Oscillation (QBO). The axial Atmospheric-Angular-Momentum (AAM) component is related to changes in LOD. Focussing on the interannual variations in the solid(More)
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