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Titlebook: Antarctic Science; Global Concerns Gotthilf Hempel Book 1994 Springer-Verlag Berlin Heidelberg 1994 Klima.Ocean.Ozone depletion.Scale.Sea i

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發(fā)表于 2025-3-21 16:34:17 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
期刊全稱(chēng)Antarctic Science
期刊簡(jiǎn)稱(chēng)Global Concerns
影響因子2023Gotthilf Hempel
視頻videohttp://file.papertrans.cn/159/158190/158190.mp4
圖書(shū)封面Titlebook: Antarctic Science; Global Concerns Gotthilf Hempel Book 1994 Springer-Verlag Berlin Heidelberg 1994 Klima.Ocean.Ozone depletion.Scale.Sea i
影響因子Public awareness of the importance of Antarctic research, particularly in relation to global problems, has increased. The book spans a broad spectrum of Antarctic science from the "ozone hole" to microbiology to the sea ice. The main focus is on the role of Antarctica and the Southern Ocean in the world climate system, e.g. the formation of sea ice and its relevance to ocean circulation, the biological pump in relation to CO2 release. The past climate history is revealed by the analysis of ice cores and sediments. Studies of plate tectonics and fossil records reach further back in earth history. Key words in the biological chapters are krill and the rich Antarctic benthos. Finally, the potential conflict between conservationists, researchers and tourists is discussed.
Pindex Book 1994
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Conflicts of Interest in the Use of Antarctica,Antarctic Treaty of 1961 acknowledges the important contribution of science. The pre-eminent position accorded to science has been vindicated: 30 years of intensive research have shown the intimate connections and controlling influences of Antarctica on the principal environmental systems of planet
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,Antarctica — Where Space Meets Planet Earth,’s environment; the atmosphere is rightly the focus of particular interest nowadays. Such changes may be either natural, such as due to volcanoes (both El Chichon in 1982 and Mount Pinatubo in 1991 put vast quantities of dust and sulphur into the lower stratosphere), or anthropogenic. Enhancement of
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The Antarctic Sea Ice Cover,from 4 million km. in summer (February) to 20 million km. in winter (September) (Zwally et al. 1983). This enormous amplitude puts Antarctic sea ice second only to Northern Hemisphere snow extent as a seasonally varying cryospheric parameter. The cycle is reasonably stable from year to year; the mos
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Detection of Change in Antarctica,interdisciplinary research theme identified by the SCAR Steering Committee (Weller et al. 1989) for the International Geosphere-Biosphere Program (IGPB) is: “., which are fundamental to establishing the current nature of trends of change and thereby providing a foundation for understanding the under
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