Abstract. We compute the polar-motion excitation function due to the atmospheric angular momentum (AAM) for both IB (inverted-barometer) and non-IB cases, as well as the excitation function from geodetically observed Earth orientation data for the period 1980-1990. The two are then compared in studying the AAM contri-bution to the polar motion excitation. The polar drifts with periods longer than--2 years have similar characteristics, but the comparison is inconclusive because of data uncertainties. For the seasonal wobble excitation, the agreement is poor except for the prograde annual wobble, indicating the influence of other geophysical excitations than AAM. For the Chandler wobble excitation, a cor-relation coefficient of 0.53 for non-I...
International audienceResults of a 100-year run of the Hadley Centre general circulation model are u...
International audienceThe interaction between the atmosphere and the underlying solid mantle is oneo...
Similar to seasonal and intraseasonal variations in polar motion (PM), interannual variations are al...
Global meteorological analyses from the European Centre for Medium Range Weather Forecasts are emplo...
Studying the planetary-dynamic behaviour of the Earth connected with geophysical processes as source...
A quantitative study on the seasonal polar motion excitated by the atmospheric angular momentum (MM)...
Analysis of nonseasonal polar motion excitation and atmospheric mass equatorial angular momentum (EA...
The inferred excitation function X-m derived from EOP(IERS 97C04) polar motion series and the series...
Changes in the annual variation of the Earth's polar motion are found to be largely caused by the va...
Aims. We investigated the causes of the Earth’s Chandler wobble variability over the past ...
International audiencePolar motion is interpreted as the effect of i) the Earths inertia moment chan...
Short periodic oscillations with the periods from 10 up to 110 days of the hemispheric components of...
Variations of the atmospheric angular momentum (AAM) is responsible for almost all of the observed l...
International audienceFrom the maps of regional contribution to atmospheric angular momentum (AAM) o...
International audienceWe analyzed the impacts of data span on trend estimates using Earth's long-ter...
International audienceResults of a 100-year run of the Hadley Centre general circulation model are u...
International audienceThe interaction between the atmosphere and the underlying solid mantle is oneo...
Similar to seasonal and intraseasonal variations in polar motion (PM), interannual variations are al...
Global meteorological analyses from the European Centre for Medium Range Weather Forecasts are emplo...
Studying the planetary-dynamic behaviour of the Earth connected with geophysical processes as source...
A quantitative study on the seasonal polar motion excitated by the atmospheric angular momentum (MM)...
Analysis of nonseasonal polar motion excitation and atmospheric mass equatorial angular momentum (EA...
The inferred excitation function X-m derived from EOP(IERS 97C04) polar motion series and the series...
Changes in the annual variation of the Earth's polar motion are found to be largely caused by the va...
Aims. We investigated the causes of the Earth’s Chandler wobble variability over the past ...
International audiencePolar motion is interpreted as the effect of i) the Earths inertia moment chan...
Short periodic oscillations with the periods from 10 up to 110 days of the hemispheric components of...
Variations of the atmospheric angular momentum (AAM) is responsible for almost all of the observed l...
International audienceFrom the maps of regional contribution to atmospheric angular momentum (AAM) o...
International audienceWe analyzed the impacts of data span on trend estimates using Earth's long-ter...
International audienceResults of a 100-year run of the Hadley Centre general circulation model are u...
International audienceThe interaction between the atmosphere and the underlying solid mantle is oneo...
Similar to seasonal and intraseasonal variations in polar motion (PM), interannual variations are al...