We develop a new method, based on interference patterns between the precession and obliquity components of geological data from Ocean Drilling Program (ODP) Leg 154 and astronomical solutions, to extract small changes in the precession constant p due to tidal dissipation over the last 25 million years and to put numerical constraints on the parameters for tidal dissipation and the dynamical ellipticity of the Earth. We show that these parameters have remained close to the present day values over the last 25 million years. The best fitting astronomical solution we obtained gives rise to a value of 0.9999 times the current day dynamical ellipticity, and 1.004 times the current day tidal dissipation value as used in the algorithm of Laskar (19...
International audienceWe present here a new solution for the astronomical computation of the insolat...
The orbital motion of the planets in the Solar System is chaotic. As a result, initially close orbit...
International audience<p>Some of the large climatic changes of the past originate in the varia...
Milankovitch band variations of past climate, inferred from the rock record, have been used to astro...
International audienceAstronomical tuning is the process of correlating geological records to an ast...
The evolution of the Solar System has been shown to be chaotic (Laskar, 1990, doi:10.1016/0019-1035(...
The correlation of Earth's orbital parameters with climatic variations has been used to generate ast...
The precession and obliquity frequencies of the Earth’s rotational motion are functions of the dynam...
Orbital tuning and understanding climate response to astronomical forcing in the Miocene require det...
International audienceThe dynamical ellipticity of a planet expresses the departure of its mass dist...
International audienceThe theoretical prediction of Earth-Moon dynamics in deep geologic time is ham...
International audienceA precise solution for the motion of the Earth axis (precession and nutation) ...
Orbital tuning and understanding climate response to astronomical forcing in the Miocene require det...
The amplitude of the Earth's nutation driven by a given component of the tidal potential is governed...
Pre-Pleistocene age models used in paleoceanography and paleoclimatology often rely on the imprint o...
International audienceWe present here a new solution for the astronomical computation of the insolat...
The orbital motion of the planets in the Solar System is chaotic. As a result, initially close orbit...
International audience<p>Some of the large climatic changes of the past originate in the varia...
Milankovitch band variations of past climate, inferred from the rock record, have been used to astro...
International audienceAstronomical tuning is the process of correlating geological records to an ast...
The evolution of the Solar System has been shown to be chaotic (Laskar, 1990, doi:10.1016/0019-1035(...
The correlation of Earth's orbital parameters with climatic variations has been used to generate ast...
The precession and obliquity frequencies of the Earth’s rotational motion are functions of the dynam...
Orbital tuning and understanding climate response to astronomical forcing in the Miocene require det...
International audienceThe dynamical ellipticity of a planet expresses the departure of its mass dist...
International audienceThe theoretical prediction of Earth-Moon dynamics in deep geologic time is ham...
International audienceA precise solution for the motion of the Earth axis (precession and nutation) ...
Orbital tuning and understanding climate response to astronomical forcing in the Miocene require det...
The amplitude of the Earth's nutation driven by a given component of the tidal potential is governed...
Pre-Pleistocene age models used in paleoceanography and paleoclimatology often rely on the imprint o...
International audienceWe present here a new solution for the astronomical computation of the insolat...
The orbital motion of the planets in the Solar System is chaotic. As a result, initially close orbit...
International audience<p>Some of the large climatic changes of the past originate in the varia...