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Salinity and the Global Water Cycle

机译:盐度与全球水循环

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Climate change is in the news frequently these days, and better-informed commentators note that changes in the water cycle pose the greatest challenge to society. We may be able to deal with an increase in temperature with a bit more air conditioning, but significant intensification in droughts and floods will be a more severe test. Civilization thrives at a range of temperatures at different latitudes, but it cannot cope without water. Thus, a number of national and international programs have been organized to assess and understand the "global water cycle." For the oceanographer, these programs have fallen short. The focus is invariably on the water cycle over land; generally, the much larger oceanic water cycle is ignored. This bias is understandable, because society's water needs are land based. But, to gauge the water cycle, it is impossible to ignore the ocean. The numbers speak for themselves: the ocean contains 97% of the free water on our planet, and 86% of the evaporation and 78% of the precipitation occurs over the ocean (Schmitt, 1995).
机译:如今,气候变化已成为新闻头条,而消息灵通的评论员指出,水循环的变化对社会构成了最大的挑战。我们也许可以通过增加一些空调来应对温度升高,但是干旱和洪水的剧烈加剧将是更严峻的考验。文明在不同纬度的温度范围内壮成长,但没有水就无法应对。因此,已经组织了许多国家和国际计划来评估和理解“全球水循环”。对于海洋学家来说,这些程序还不够。重点始终是陆地上的水循环。通常,更大的海洋水循环被忽略。这种偏见是可以理解的,因为社会的水需求是基于土地的。但是,要衡量水循环,就不可能忽视海洋。数字不言而喻:海洋中有97%的自由水来自地球,86%的蒸发和78%的降水发生在海洋上(Schmitt,1995)。

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