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- W1497404881 abstract "This chapter describes lessons learned from the study of climatic changes in the past, the corresponding large-scale reorganization of the mode of operation for the ocean-atmosphere system, and the possible linkage between climate change and ocean circulation. The cyclic climatic changes between warm and cold periods are recorded by oxygen isotope in foraminifera shells deposited in the deep sea sediments. The increase in ice volume enriches the heavier oxygen isotope in sea water, because the isotope fractionation during the evaporation of sea water preferentially sends the lighter oxygen isotope into the gas phase. This water vapor eventually precipitates from the air as snow and then becomes ice in the high latitude regions. Part of the alkalinity increases that the polar alkalinity hypothesis requires for glacial surface water in the Antarctic could be a natural consequence of the demise of the North Atlantic Deep Water (NADW) during glacial time. The cessation of NADW stopped the flow of low-alkalinity deep water into the circumpolar region. The most important feature of the ocean conveyor circulation is the production of deep water in the northern Atlantic. Waters in the vicinity of Iceland are cooled and their density is increased to the point that they sink into the abyss." @default.
- W1497404881 created "2016-06-24" @default.
- W1497404881 creator A5057798665 @default.
- W1497404881 date "1995-01-01" @default.
- W1497404881 modified "2023-09-27" @default.
- W1497404881 title "Future climate surprises" @default.
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- W1497404881 doi "https://doi.org/10.1016/s0168-6321(06)80037-4" @default.
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