作者: 羞辱 時(shí)間: 2025-3-22 00:08
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 作者: countenance 時(shí)間: 2025-3-22 00:38 作者: Anthrp 時(shí)間: 2025-3-22 07:02 作者: 珠寶 時(shí)間: 2025-3-22 11:04 作者: 無王時(shí)期, 時(shí)間: 2025-3-22 15:41 作者: 無王時(shí)期, 時(shí)間: 2025-3-22 20:39 作者: fulmination 時(shí)間: 2025-3-22 22:32
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 作者: BARB 時(shí)間: 2025-3-23 02:27 作者: 拋物線 時(shí)間: 2025-3-23 07:10
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作者: 滲入 時(shí)間: 2025-3-23 23:22 作者: 圣人 時(shí)間: 2025-3-24 05:40 作者: Thyroxine 時(shí)間: 2025-3-24 10:19 作者: 一個(gè)姐姐 時(shí)間: 2025-3-24 13:47
Response of Italian Glaciers to Climatic VariationsThe glaciers of the southern alpine slope have been investigated using a variety of different methods. The most common ones are:作者: 色情 時(shí)間: 2025-3-24 16:40 作者: 可行 時(shí)間: 2025-3-24 19:40 作者: ANTE 時(shí)間: 2025-3-24 23:26 作者: 共同生活 時(shí)間: 2025-3-25 06:37
Introduction to Electron Beam Instruments,luid plays an insignificant role in the transportation of momentum, flows of such materials can be considered as dispersed single-phase flows. In other occasions, when the mass of the interstitial fluid is comparable to that of the solids the interactions between the fluid and solid phases are signi作者: CLOT 時(shí)間: 2025-3-25 11:08
https://doi.org/10.1007/978-1-4899-1522-1ological and geophysical observations of the Earth’s surface, its relative horizontal motions and its topography. Direct consequences of the mantle flow include plate tectonics, which refers to the relative motions of the continents, spreading of the sea-floor, creation of new crust and mid-ocean ri作者: HAVOC 時(shí)間: 2025-3-25 15:39 作者: 原來 時(shí)間: 2025-3-25 19:06 作者: 審問 時(shí)間: 2025-3-25 20:18
Václav Drchal,Václav Jani?,Josef Kudrnovskyhis massive amount of material is subsequently deposited on the ground, with much of the coarser fraction of the flow being deposited within a few hundred kilometres of the volcanic edifice. This may lead to a substantial regional change to the topography, with ash flow deposits being tens to hundre作者: 糾纏,纏繞 時(shí)間: 2025-3-26 03:01 作者: 聯(lián)想 時(shí)間: 2025-3-26 04:54 作者: expound 時(shí)間: 2025-3-26 11:41 作者: 細(xì)絲 時(shí)間: 2025-3-26 15:48 作者: 祖?zhèn)髫?cái)產(chǎn) 時(shí)間: 2025-3-26 16:48
W. Dekeyser,L. Fiermans,J. Vennikplitudes of these disastrous events appear to have increased in recent years perhaps due to recent climate warming. The events endanger the personal property and infra-structure in mountainous regions. For example, from the winters 1940/41 to 1987/88 more than 7000 snow avalanches occurred in Switze作者: 大方一點(diǎn) 時(shí)間: 2025-3-26 21:31 作者: 消息靈通 時(shí)間: 2025-3-27 04:39
https://doi.org/10.1007/978-1-4757-5099-7es subject to a free surface flow bounded by a granular medium. Flow of water also occurs very slowly through the interstices of the granular medium: however such a weak filtration process may be safely ignored. The interface between flowing mixture and granular medium can move as a result of a cont作者: V洗浴 時(shí)間: 2025-3-27 07:24 作者: manifestation 時(shí)間: 2025-3-27 12:59 作者: POLYP 時(shí)間: 2025-3-27 15:46 作者: 侵略主義 時(shí)間: 2025-3-27 20:33
https://doi.org/10.1007/3-540-45670-8Geomorphology; Iceberg; convection; dynamics; fluid mechanics; geophysics; granular matter; material; mud fl作者: 盟軍 時(shí)間: 2025-3-27 23:23
https://doi.org/10.1007/978-1-4899-1370-8 the properties of such fluids. In the current chapter, we go further in this direction and describe more developments of a theoretical model for lava flows. Lava flows have recently been the subject of a review by Griffiths [.] (see also Chap. 6). Our aim here is to illustrate the use of viscoplastic rheological models in this problem.作者: 怪物 時(shí)間: 2025-3-28 06:10
https://doi.org/10.1007/978-1-4757-5099-7es subject to a free surface flow bounded by a granular medium. Flow of water also occurs very slowly through the interstices of the granular medium: however such a weak filtration process may be safely ignored. The interface between flowing mixture and granular medium can move as a result of a continuous exchange of sediment particles. The .’.作者: declamation 時(shí)間: 2025-3-28 06:50 作者: anticipate 時(shí)間: 2025-3-28 11:33 作者: faultfinder 時(shí)間: 2025-3-28 15:59
16 Invitation to Sediment Transportes subject to a free surface flow bounded by a granular medium. Flow of water also occurs very slowly through the interstices of the granular medium: however such a weak filtration process may be safely ignored. The interface between flowing mixture and granular medium can move as a result of a continuous exchange of sediment particles. The .’.作者: FLIP 時(shí)間: 2025-3-28 20:57
Dunes and Drumlinswind blows sand into a wide variety of different shapes (see Chap. 17 for many illustration of such dunes). Linear dunes, or ‘seifs’, are ridges which form parallel to the prevailing wind direction, while transverse dunes are ridges perpendicular to the wind. A variety of other shapes can occur, amongst them star dunes and barchan dunes.作者: ethnology 時(shí)間: 2025-3-29 02:45 作者: Diastole 時(shí)間: 2025-3-29 03:15
Geophysical Aspects of Non-Newtonian Fluid Mechanicsan Fluid Mechanics, Rheologica Acta, Journal of Fluid Mechanics, Journal of Rheology, amongst others). It is an area of active research, both for industrial fluid problems and for applications elsewhere, notably geophysically motivated issues such as the flow of lava and ice, mud slides, snow avalan作者: Omniscient 時(shí)間: 2025-3-29 11:13
Introduction to Rheology and Application to Geophysicsor each topic considered here, we will outline the key elements and point the reader to ward the most helpful references and authoritative works. The reader is also referred to available books introducing rheology [.],[.] for a more complete presentation and to the tutorial written by Middleton and 作者: 暴發(fā)戶 時(shí)間: 2025-3-29 12:27
Granular Material Theories Revisitedluid plays an insignificant role in the transportation of momentum, flows of such materials can be considered as dispersed single-phase flows. In other occasions, when the mass of the interstitial fluid is comparable to that of the solids the interactions between the fluid and solid phases are signi作者: choleretic 時(shí)間: 2025-3-29 18:05
Earth’s Surface Morphology and Convection in the Mantleological and geophysical observations of the Earth’s surface, its relative horizontal motions and its topography. Direct consequences of the mantle flow include plate tectonics, which refers to the relative motions of the continents, spreading of the sea-floor, creation of new crust and mid-ocean ri作者: Madrigal 時(shí)間: 2025-3-29 19:50
Morphological Instabilities in Flows with Cooling, Freezing or Dissolutioneither within the crust or as surface lava flows, and the way in which these flows are affected by variable viscosity due to cooling or by a yield strength resulting fromsolidification. These effects invariably lead to non-uniformor three-dimensional flow patterns, particularly fingering and channel作者: 蕁麻 時(shí)間: 2025-3-30 00:42
Shallow Lava Theory the properties of such fluids. In the current chapter, we go further in this direction and describe more developments of a theoretical model for lava flows. Lava flows have recently been the subject of a review by Griffiths [.] (see also Chap. 6). Our aim here is to illustrate the use of viscoplast作者: Obsequious 時(shí)間: 2025-3-30 04:12
Explosive Volcanic Eruptionshis massive amount of material is subsequently deposited on the ground, with much of the coarser fraction of the flow being deposited within a few hundred kilometres of the volcanic edifice. This may lead to a substantial regional change to the topography, with ash flow deposits being tens to hundre作者: 統(tǒng)治人類 時(shí)間: 2025-3-30 10:13
The Dynamics of Snow and Ice Massese than two-thirds of the surface of Earth is covered by water, it is the water to ice conversion, and vice versa, that makes an important fraction of the globe habitable today. Hence, changes in the global scale dynamics of the ice cover capture scientific and public interest principally because of 作者: 精密 時(shí)間: 2025-3-30 13:44 作者: olfction 時(shí)間: 2025-3-30 19:58 作者: debris 時(shí)間: 2025-3-30 21:43
Snow Avalanchesransportation, construction in high altitude areas, etc. In these mountain ranges, avalanches often threaten man’s activities and life. Typical examples include recent disasters, such as the avalanche at Val d’Isère in 1970 (39 people were killed in a hostel) or the series of catastrophic avalanches作者: 核心 時(shí)間: 2025-3-31 00:59
Dense Granular Avalanches: Mathematical Description and Experimental Validationplitudes of these disastrous events appear to have increased in recent years perhaps due to recent climate warming. The events endanger the personal property and infra-structure in mountainous regions. For example, from the winters 1940/41 to 1987/88 more than 7000 snow avalanches occurred in Switze作者: angiography 時(shí)間: 2025-3-31 05:44 作者: FIS 時(shí)間: 2025-3-31 11:10 作者: AWRY 時(shí)間: 2025-3-31 15:44 作者: 礦石 時(shí)間: 2025-3-31 20:30
Dunes and Drumlinswind blows sand into a wide variety of different shapes (see Chap. 17 for many illustration of such dunes). Linear dunes, or ‘seifs’, are ridges which form parallel to the prevailing wind direction, while transverse dunes are ridges perpendicular to the wind. A variety of other shapes can occur, amo作者: 殺菌劑 時(shí)間: 2025-3-31 22:39 作者: 散步 時(shí)間: 2025-4-1 04:27
Book 2001re 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作者: FILLY 時(shí)間: 2025-4-1 06:12 作者: EVICT 時(shí)間: 2025-4-1 12:47
C. A. Frishberg,M. J. Goldberg,L. J. Massat features of avalanches (formation and motion) and outlines the main approaches used for describing their movement. We do not tackle specific problems related to snow mechanics and avalanche forecasting. For more information on the subject, the reader is referred to the main textbooks published in Alpine countries [.],[.],[.],[.],[.],[.],[.],[.].作者: 偏離 時(shí)間: 2025-4-1 16:33 作者: endoscopy 時(shí)間: 2025-4-1 19:40
Geophysical Aspects of Non-Newtonian Fluid Mechanicsral textbooks are useful sources of information; for example, [.],[.],[.] are standard texts giving mathematical and engineering perspectives upon the subject. In these lecture notes, Ancey’s chapter on rheology (Chap. 3) gives further introduction.作者: choleretic 時(shí)間: 2025-4-1 22:41
Snow Avalanchest features of avalanches (formation and motion) and outlines the main approaches used for describing their movement. We do not tackle specific problems related to snow mechanics and avalanche forecasting. For more information on the subject, the reader is referred to the main textbooks published in Alpine countries [.],[.],[.],[.],[.],[.],[.],[.].作者: indigenous 時(shí)間: 2025-4-2 03:16 作者: 確認(rèn) 時(shí)間: 2025-4-2 10:16 作者: 失望未來 時(shí)間: 2025-4-2 12:57
Neepa T. Maitra,Adam Wasserman,Kieron Burkethe globe habitable today. Hence, changes in the global scale dynamics of the ice cover capture scientific and public interest principally because of their role in global warming and ice-age events. It is in this sense that ice is the ultimate geomorphological fluid mechanic.
