The Great Season Climatic Oscillation

Abstract

The variations of water density and thermal conductivity of the oceans cold region waters according to their salinity lead to suggest an hypothesis of an oscillating climate between two extreme positions: a maximum of hot temperatures and a minimum of cold ones. It will be shown that the distance separating the surface hot streams from the depth cold ones oscillate between two limit values linked to the optimal melting and regeneration glaciers. The melting and regeneration glaciers cycle leads to the Great Saison Climatic Oscillations phenomenon necessary to the regeneration of fresh water resources of our planet.