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Titlebook: Ice Ages and Interglacials; Measurements, Interp Donald Rapp Book 20091st edition Springer-Verlag Berlin Heidelberg 2009 Ice ages.Interglac

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發(fā)表于 2025-3-21 19:22:05 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Ice Ages and Interglacials
副標(biāo)題Measurements, Interp
編輯Donald Rapp
視頻videohttp://file.papertrans.cn/461/460699/460699.mp4
概述Provides an independent and complete summary of the latest data on ice ages.Explores theories and makes comparisons with the all the available data.Acts as a primary textbook on ice ages and a seconda
叢書名稱Springer Praxis Books
圖書封面Titlebook: Ice Ages and Interglacials; Measurements, Interp Donald Rapp Book 20091st edition Springer-Verlag Berlin Heidelberg 2009 Ice ages.Interglac
描述.Ice ages represent perhaps the most dramatic example of extreme climate change on the Earth. Understanding how and why ice ages occur is of great importance in our wider understanding of the global climate system and how it might change. If one examines Greenland ice data for the past 100,000 years, it becomes very clear that the relatively warm period of the past 11,000 years stand out in striking contrast to the 90,000 years of extreme cold that preceded it. We now refer to the unusually warm period that we are in at the present time as an interglacial; the long preceding period of cold is a glacial or ice age. During the last ice age, humans developed elaborate tools and homo sapiens migrated from Africa to Europe, but it wasn’t until that ice age ended 11,000 years ago that agriculture began and with it the foundation of modern civilization. It is therefore not surprising that there is enormous interest in trying to work out the mechanisms which trigger ice ages to begin, and what causes them to end. Of particular interest is the fact that ice ages appear to begin and end very abruptly on the geological timescale. ...Previous and existing books on ice ages are mostly short, po
出版日期Book 20091st edition
關(guān)鍵詞Ice ages; Interglacials; Interpretation models; Ocean; Snow; Sustainable development; biosphere; climate ch
版次1
doihttps://doi.org/10.1007/978-3-540-89680-7
isbn_softcover978-3-642-10051-2
isbn_ebook978-3-540-89680-7
copyrightSpringer-Verlag Berlin Heidelberg 2009
The information of publication is updating

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,Variability of the Earth’s climate,he rate at which energy is released from the interior of the Earth is 3.1×10. kW. The solar power that impinges on the Earth is 342 W/m.. If all of this were absorbed, the Earth would receive 1.7×10. kW. Actually, only about 70% of incident solar energy is absorbed by the Earth; nevertheless the sol
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Ice core data,ly existent on Earth are located where landmasses exist near the poles: Greenland and Antarctica. Both ice sheets store a huge amount of water, as indicated in Table 4.1. If the Antarctic ice sheet were to fully melt, the ocean level would rise about 68 meters. Full melting of the Greenland ice shee
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Summary of climate variations,, a circumpolar ocean current developed around Antarctica which thermally isolated it, allowing glaciation to proceed. In addition, there may have been a reduction in atmospheric CO.. Mountain building may have hastened glaciation. Since about 34 million years ago, the temperature of the Earth has b
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Comparison of astronomical theory with data,ly small percentage changes that occur in solar intensity are sufficient to cause major changes in global climate. However, this question is complicated by the possibility that large positive feedback forcings (albedo, ocean currents, wind changes, etc.) might be initiated by smaller changes in sola
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