Oceanic contributions to the seasonal wobbles of polar motion are evaluated using three different ocean circulation models: (a) the POCM (Parallel Ocean Climate Model); (b) the model by Ponte et al. (1998); (c) the model by Thomas and Suendermann (1998). The excitation ellipses are given at annual, semi-annual and thrice-yearly periods. These ellipse parameters are compared to differences: (excitation from observations) - (atmospheric part). The model by Ponte et al. nearly closes the balance. (orig.)SIGLEAvailable from TIB Hannover: RR 6134(99/10) / FIZ - Fachinformationszzentrum Karlsruhe / TIB - Technische InformationsbibliothekDEGerman
International audienceThe terrestrial motion of the Earth's rotation pole shows mainly two large osc...
Polar motion excitation involves mass redistributions and motions of the Earth system relative to th...
Recent numerical simulations using global ocean circulation models are reviewed together with model ...
Recent studies based on various ocean general circulation models (OGCMs) demonstrate that the oceans...
A number of ocean models of different complexity have been used to study changes in the oceanic angu...
Abstract. This paper describes the use of a global numerical model of the oceans to estilnate variat...
The global oceans play important roles in exciting the annual polar motion besides the atmosphere. H...
[1] Mass redistribution and motion in the oceans are major driving forces of geodetic variations, in...
We revisit the problem of modeling the ocean’s contribution to rapid, non-tidal Earth rotation varia...
Similar to seasonal and intraseasonal variations in polar motion (PM), interannual variations are al...
Changes in the oceanic current system and in the oceanic mass distribution alter the state of the Ea...
Terrestrial water storage (TWS) and ocean bottom pressure (OBP) are major contributors to the observ...
Changes in the annual variation of the Earth's polar motion are found to be largely caused by the va...
A quantitative study on the seasonal polar motion excitated by the atmospheric angular momentum (MM)...
The oceanic contribution to Earth rotation anomalies can be manifold. Possible causes are a change o...
International audienceThe terrestrial motion of the Earth's rotation pole shows mainly two large osc...
Polar motion excitation involves mass redistributions and motions of the Earth system relative to th...
Recent numerical simulations using global ocean circulation models are reviewed together with model ...
Recent studies based on various ocean general circulation models (OGCMs) demonstrate that the oceans...
A number of ocean models of different complexity have been used to study changes in the oceanic angu...
Abstract. This paper describes the use of a global numerical model of the oceans to estilnate variat...
The global oceans play important roles in exciting the annual polar motion besides the atmosphere. H...
[1] Mass redistribution and motion in the oceans are major driving forces of geodetic variations, in...
We revisit the problem of modeling the ocean’s contribution to rapid, non-tidal Earth rotation varia...
Similar to seasonal and intraseasonal variations in polar motion (PM), interannual variations are al...
Changes in the oceanic current system and in the oceanic mass distribution alter the state of the Ea...
Terrestrial water storage (TWS) and ocean bottom pressure (OBP) are major contributors to the observ...
Changes in the annual variation of the Earth's polar motion are found to be largely caused by the va...
A quantitative study on the seasonal polar motion excitated by the atmospheric angular momentum (MM)...
The oceanic contribution to Earth rotation anomalies can be manifold. Possible causes are a change o...
International audienceThe terrestrial motion of the Earth's rotation pole shows mainly two large osc...
Polar motion excitation involves mass redistributions and motions of the Earth system relative to th...
Recent numerical simulations using global ocean circulation models are reviewed together with model ...