大季节气候振荡
The Great Season Climatic Oscillation
摘要：
海洋冷区水的密度和热导系数随盐度的变化，提出了一种假设，即气候在两个极端位置之间振荡：最高热温度和最低冷温度。它将被证明，从深度冷的表面热流分离的距离振荡之间的两个极限值链接到最佳的融化和再生冰川。冰川的融化和再生循环导致了大季节气候振荡现象，这是我们星球淡水水资源再生所必需的。
英文摘要：
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.
机构、总结、中文摘要均由AI分析而来，可能存在错误，请以论文正文为准。
