The gigantic thermal machine. So how does this main forcing of the Sun function ? External Forcing of the climate: variations in the orbital parameters of the Earth (Milankovitch’s theory)

La grande machine climatique. Comment le forçage principal, le Soleil, se comporte-t-il ? Variations des paramètres orbitaux de la Terre : Thérorie de Milankovitch

The previous interglacial (Marine isotope stage 5e, peaking at 125 kyr BP) is usually assumed to be a good analogue for our present-day climate. Moreover, as our present interglacial, the Holocene, is

The European Science Foundation (ESF) and the French Foundation of the Maison des Sciences de l’Homme (FMSH) (within the Entre-Sciences programme) have agreed to jointly develop a new conference

Data show that climate has always changed in the past, sometimes with a larger amplitude than what we experimented for two decades. But the main signatures of the anthopogenic forcing are the speed of

The European Science Foundation (ESF) and the French Foundation of the Maison des Sciences de l’Homme (FMSH) (within the Entre-Sciences programme) have agreed to jointly develop a new conference