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Titlebook: Geomorphological Fluid Mechanics; N. J. Balmforth,A. Provenzale Book 2001 Springer-Verlag Berlin Heidelberg 2001 Geomorphology.Iceberg.con

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發(fā)表于 2025-3-21 17:49:28 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Geomorphological Fluid Mechanics
編輯N. J. Balmforth,A. Provenzale
視頻videohttp://file.papertrans.cn/384/383866/383866.mp4
概述Bridges the gap between textbook material and forefront research
叢書名稱Lecture Notes in Physics
圖書封面Titlebook: Geomorphological Fluid Mechanics;  N. J. Balmforth,A. Provenzale Book 2001 Springer-Verlag Berlin Heidelberg 2001 Geomorphology.Iceberg.con
描述Geomorphology deals with some of the most striking patterns of nature. From mountain ranges and mid-ocean ridges to river networks and sand dunes, there is a whole family of forms, structures, and shapes that demand rationalization as well as mathematical description. In the various chapters of this volume, many of these patterns are explored and discussed, and attempts are made to both unravel the reasons for their very existence and to describe their dynamics in quantitative terms. Particular focus is placed on lava and mud flows, ice and snow dynamics, river and coastal morphodynamics and landscape formation. Combining a pedagogical approach with up-to-date reviews of forefront research, this volume will serve both postgraduate students and lecturers in search of advanced textbook material, and experienced researchers wishing to get acquainted with the various physical and mathematical approaches in a range of closely related research fields.
出版日期Book 2001
關(guān)鍵詞Geomorphology; Iceberg; convection; dynamics; fluid mechanics; geophysics; granular matter; material; mud fl
版次1
doihttps://doi.org/10.1007/3-540-45670-8
isbn_softcover978-3-642-07693-0
isbn_ebook978-3-540-45670-4Series ISSN 0075-8450 Series E-ISSN 1616-6361
issn_series 0075-8450
copyrightSpringer-Verlag Berlin Heidelberg 2001
The information of publication is updating

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https://doi.org/10.1007/978-1-4899-1522-1hology because they are responsible for producing much of the large-scale topography (horizontally > 10 km) of the Earth’s surface. This topography, in turn, imposes strong influences on the atmosphere and ocean circulation patterns, affects precipitation, and provides the base on which erosion and
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Earth’s Surface Morphology and Convection in the Mantlehology because they are responsible for producing much of the large-scale topography (horizontally > 10 km) of the Earth’s surface. This topography, in turn, imposes strong influences on the atmosphere and ocean circulation patterns, affects precipitation, and provides the base on which erosion and
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Asymptotic Theories of Ice Sheets and Ice Shelves the mean temperature of the Earth’s surface is immense, it is absolutely vital that the nourishment and wastage of the large ice masses are properly understood and transformed into sea level status. This requires careful computation of the flow, phase change mechanisms as well as geometric evolutio
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