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Titlebook: Climate, Earth Processes and Earth History; Richard John Huggett Book 1991 Springer-Verlag Berlin Heidelberg 1991 Erdgeschichte.Geomorphol

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發(fā)表于 2025-3-21 17:31:25 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Climate, Earth Processes and Earth History
編輯Richard John Huggett
視頻videohttp://file.papertrans.cn/228/227681/227681.mp4
圖書封面Titlebook: Climate, Earth Processes and Earth History;  Richard John Huggett Book 1991 Springer-Verlag Berlin Heidelberg 1991 Erdgeschichte.Geomorphol
描述Today, climate-related processes and problems are referred to as Global Change by nearly everyone including scientists, politicians, and economists; citizens worldwide are anxious about the often ob- served disorientation of our environment under the influence of man. Better information on the Earth‘s natural systems and their possible alterations is necessary. The topic itself is so wide that sound scien- tific descriptions of it as a whole are rare. For the non-specialist infor- mation from relevant fields is not easy to obtain; and often, the pro- gnostic models presented are contradictory and even for specialists difficult to evaluate. Therefore, this book on Climate, Earth Processes and Earth History by Richard Huggett fills an important gap. It discusses the great, climate-related areas of the Earth‘s environment. The atmosphere, the hydrosphere, the sediments as products of weathering and geomorphic processes, the relief as landforms and soils, and the biosphere are thoroughly treated as the prominent sub- systems which are greatly affected by climate. These subsystems not only control the visual and internal aspects of our landscapes, but they are themselves especially infl
出版日期Book 1991
關(guān)鍵詞Erdgeschichte; Geomorphologie; Klima; Sediment; biosphere; climate; earth history; earth surface systems; ge
版次1
doihttps://doi.org/10.1007/978-3-642-76268-0
isbn_softcover978-3-642-76270-3
isbn_ebook978-3-642-76268-0
copyrightSpringer-Verlag Berlin Heidelberg 1991
The information of publication is updating

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Air,alilei observed them through his telescope around 1611, since soon after which time they have been surveyed more or less continuously. A German apothecary and amateur solar observer, Heinrich S. Schwabe, suspected from his observations over the years 1826 to 1837 that the number of spots on the sola
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Sediments,–31) in a paper concerned with the formation of alluvial deposits, and in a report by John Phillips (1831) entitled .. Chemical weathering was discussed in Karl Gustav Christoph Bischof’s monumental book . (1854–59). During the 1860s, students of weathering became more vocal, perhaps spurred on by t
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Landforms and Soils,ter levels in soils. A fuller appreciation of the climatic factor in soil formation has been attributed to Johann Christian Hundeshagen who, in his . (1830–32), mentioned that the climatic forces —water, heat, light, and oxygen—must act in unison to create a productive soil (Joffe 1949, p. 12). G.C.
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Animals and Plants,o flourished between the third and fifth centuries .... Menestor, in the fifth century ...., was aware of a correlation between the evergreen and deciduous habits of vegetation and climate (Morton 1981). The first major treatise on plant geography and ecology was dished up by Theophrastus (370–385 .
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Biomes and Zonobiomes,er. Notions of the “plenitude of Nature”, food chains, and equilibrium of numbers were first grappled with by some of the most celebrated natural historians of the eighteenth century, such as Carl Linneaus, as well as by men no less great but not so well known in their day, such as Gilbert White of
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Artinian rings with Morita duality (I),alilei observed them through his telescope around 1611, since soon after which time they have been surveyed more or less continuously. A German apothecary and amateur solar observer, Heinrich S. Schwabe, suspected from his observations over the years 1826 to 1837 that the number of spots on the sola
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