The Great Season Climatic Oscillation

dc.creatorBoucenna, Ahmed
dc.date2007-01-24
dc.date2007-02-12
dc.date.accessioned2026-07-07T07:46:02Z
dc.date.available2026-07-07T07:46:02Z
dc.descriptionThe 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.
dc.description8 pages
dc.identifierhttps://arxiv.org/abs/physics/0701283
dc.identifierhttp://arxiv.org/abs/physics/0701283
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/123698
dc.subjectAtmospheric and Oceanic Physics
dc.titleThe Great Season Climatic Oscillation
dc.typetext

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