標(biāo)題: Titlebook: Dynamics of Ice Sheets and Glaciers; Ralf Greve,Heinz Blatter Book 2009 Springer-Verlag Berlin Heidelberg 2009 Geophysics.dynamics.flow.gl [打印本頁] 作者: Curator 時(shí)間: 2025-3-21 17:03
書目名稱Dynamics of Ice Sheets and Glaciers影響因子(影響力)
書目名稱Dynamics of Ice Sheets and Glaciers影響因子(影響力)學(xué)科排名
書目名稱Dynamics of Ice Sheets and Glaciers網(wǎng)絡(luò)公開度
書目名稱Dynamics of Ice Sheets and Glaciers網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Dynamics of Ice Sheets and Glaciers被引頻次
書目名稱Dynamics of Ice Sheets and Glaciers被引頻次學(xué)科排名
書目名稱Dynamics of Ice Sheets and Glaciers年度引用
書目名稱Dynamics of Ice Sheets and Glaciers年度引用學(xué)科排名
書目名稱Dynamics of Ice Sheets and Glaciers讀者反饋
書目名稱Dynamics of Ice Sheets and Glaciers讀者反饋學(xué)科排名
作者: custody 時(shí)間: 2025-3-21 23:05
978-3-642-26935-6Springer-Verlag Berlin Heidelberg 2009作者: 現(xiàn)暈光 時(shí)間: 2025-3-22 00:28
Dynamics of Ice Sheets and Glaciers978-3-642-03415-2Series ISSN 1866-8348 Series E-ISSN 1866-8356 作者: eulogize 時(shí)間: 2025-3-22 05:09 作者: FEAS 時(shí)間: 2025-3-22 08:52
Well-Being, Paid Work and Personal Lifeor ice shelves of Antarctica (Ross Ice Shelf, Filchner-R?nne Ice Shelf, Amery Ice Shelf), are confined by large embayments. Smaller ice shelves can also be unconfined. In the latter case, stabilisation typically results from the contact with small islands or grounding on shoals.作者: Camouflage 時(shí)間: 2025-3-22 15:42 作者: Camouflage 時(shí)間: 2025-3-22 17:15
Large-Scale Dynamics of Ice Shelves,or ice shelves of Antarctica (Ross Ice Shelf, Filchner-R?nne Ice Shelf, Amery Ice Shelf), are confined by large embayments. Smaller ice shelves can also be unconfined. In the latter case, stabilisation typically results from the contact with small islands or grounding on shoals.作者: Ingest 時(shí)間: 2025-3-23 00:38 作者: BALE 時(shí)間: 2025-3-23 04:39
Advances in Geophysical and Environmental Mechanics and Mathematicshttp://image.papertrans.cn/e/image/284096.jpg作者: colostrum 時(shí)間: 2025-3-23 09:17 作者: 出價(jià) 時(shí)間: 2025-3-23 10:59
The Politico-Economic Dimension is an abstract definition which has many possible realisations (numbers, functions, geometric objects and so on). For our purposes, it is sufficient to consider one of them, namely the geometric object of an . in the three-dimensional, Euclidian, physical space .. Therefore, in our sense a vector a作者: 勾引 時(shí)間: 2025-3-23 15:16
Realism, Internationalism, Globalismaterial elements, called .. For any time ., each particle is identified by a position vector x (relative to a prescribed origin .) in the physical space ., and the continuous set of position vectors for all particles of the body is called a . of the body. If . is the actual time, the corresponding c作者: CURB 時(shí)間: 2025-3-23 20:25
Well-Being, Paid Work and Personal Lifels, that is, the water molecules are arranged in layers of hexagonal rings (Fig. 4.1). The plane of such a layer is called the ., which actually consists of two planes shifted slightly (by 0.0923?nm) against each other. The direction perpendicular to the basal planes is the . or ., and the distance 作者: Transfusion 時(shí)間: 2025-3-24 02:14
Judith Sixsmith,Margaret Bonehamlow of ice in an ice sheet. Figure 5.1 shows the typical geometry (cross section) of a grounded ice sheet with attached floating ice shelf (the latter will be treated in Chap. 6), as well as its interactions with the atmosphere (snowfall, melting), the lithosphere (geothermal heat flux, isostasy) an作者: handle 時(shí)間: 2025-3-24 03:56 作者: 大方一點(diǎn) 時(shí)間: 2025-3-24 10:18
Dimitris Ballas,Danny Dorling,Mary Shawilometres in diameter down to small glaciers of a few hundreds of metres in length. Consequently, the scaling given for ice sheets in Chapter 5 [Eqs. (5.5) and (5.102)] is not valid for smaller ice caps and glaciers, and needs to be modified. However, the Froude number (5.7) and Coriolis-force-to-pr作者: fringe 時(shí)間: 2025-3-24 13:32
‘Anglo-America’ and Atlantic Europer only in Antarctica and Greenland, whereas during the Last Glacial Maximum (LGM), 21,000 years ago, extended ice sheets also covered large parts of North America, northern Europe, etc. (see Chapter 1). These ice sheets, with typical thicknesses of several kilometres, impose therefore large, time-de作者: acrimony 時(shí)間: 2025-3-24 15:03
‘Anglo-America’ and Atlantic Europetopics at the forefront of current research. The selection of the topics (induced anisotropy, compressible firn, polythermal glaciers) is strongly influenced by the authors’ own research interests and makes no claim to be complete. Other issues, such as subglacial hydrology, ice stream dynamics or c作者: Coma704 時(shí)間: 2025-3-24 20:25
‘Anglo-America’ and Atlantic EuropeIn agreement with the scope of the series . (AGEM.), it is our intention that this book serves the purposes作者: 橫截,橫斷 時(shí)間: 2025-3-25 02:56 作者: rectocele 時(shí)間: 2025-3-25 05:44
1866-8348 linear algebra) and physics (classical mechanics, thermodynamics) provide a sufficient background for successfully studying the text..978-3-642-26935-6978-3-642-03415-2Series ISSN 1866-8348 Series E-ISSN 1866-8356 作者: 賞心悅目 時(shí)間: 2025-3-25 09:35 作者: Engulf 時(shí)間: 2025-3-25 12:27 作者: 象形文字 時(shí)間: 2025-3-25 19:36 作者: miniature 時(shí)間: 2025-3-25 22:41 作者: Parallel 時(shí)間: 2025-3-26 04:06 作者: GREEN 時(shí)間: 2025-3-26 05:53 作者: neolith 時(shí)間: 2025-3-26 12:18
Dynamics of Glacier Flow,ilometres in diameter down to small glaciers of a few hundreds of metres in length. Consequently, the scaling given for ice sheets in Chapter 5 [Eqs. (5.5) and (5.102)] is not valid for smaller ice caps and glaciers, and needs to be modified. However, the Froude number (5.7) and Coriolis-force-to-pr作者: JUST 時(shí)間: 2025-3-26 12:50 作者: 發(fā)源 時(shí)間: 2025-3-26 19:55
Advanced Topics,topics at the forefront of current research. The selection of the topics (induced anisotropy, compressible firn, polythermal glaciers) is strongly influenced by the authors’ own research interests and makes no claim to be complete. Other issues, such as subglacial hydrology, ice stream dynamics or c作者: GLOOM 時(shí)間: 2025-3-26 23:14
Book 2009f general continuum mechanics, the different initial-boundary-value problems for the flow of ice sheets, ice shelves, ice caps and glaciers are systematically derived. Special emphasis is put on developing hierarchies of approximations for the different systems, and suitable numerical solution techn作者: FLAX 時(shí)間: 2025-3-27 02:56 作者: 多節(jié) 時(shí)間: 2025-3-27 07:21 作者: insurgent 時(shí)間: 2025-3-27 13:01
‘Anglo-America’ and Atlantic Europeorth America, northern Europe, etc. (see Chapter 1). These ice sheets, with typical thicknesses of several kilometres, impose therefore large, time-dependent loads on the crust of the Earth, to which the body of the Earth as a visco-elastic, multi-layer system reacts with a delayed, essentially vertical displacement.作者: CIS 時(shí)間: 2025-3-27 15:11 作者: 誰在削木頭 時(shí)間: 2025-3-27 18:43
Elements of Continuum Mechanics,ce ., and the continuous set of position vectors for all particles of the body is called a . of the body. If . is the actual time, the corresponding configuration is called the ... In addition, we define a .. which refers to a fixed (or initial) time ...作者: Fester 時(shí)間: 2025-3-27 22:09
Glacial Isostasy,orth America, northern Europe, etc. (see Chapter 1). These ice sheets, with typical thicknesses of several kilometres, impose therefore large, time-dependent loads on the crust of the Earth, to which the body of the Earth as a visco-elastic, multi-layer system reacts with a delayed, essentially vertical displacement.作者: Spartan 時(shí)間: 2025-3-28 06:04 作者: Cultivate 時(shí)間: 2025-3-28 06:34 作者: nepotism 時(shí)間: 2025-3-28 13:45 作者: Infelicity 時(shí)間: 2025-3-28 18:11 作者: 性別 時(shí)間: 2025-3-28 22:47 作者: 性上癮 時(shí)間: 2025-3-28 23:34 作者: 財(cái)主 時(shí)間: 2025-3-29 03:22 作者: 巧辦法 時(shí)間: 2025-3-29 10:08
Ice in the Climate System,sed by large bays. Extended land-based masses of ice covering less than 50,000?km. are termed ice caps, and smaller ice masses constrained by topographical features (for instance a mountain valley) are called glaciers. Sea ice floats on the ocean; however, in contrast to an ice shelf it forms directly by freezing sea water.作者: 宏偉 時(shí)間: 2025-3-29 14:42 作者: 按時(shí)間順序 時(shí)間: 2025-3-29 18:02
Dynamics of Glacier Flow,essure-gradient ratio (5.10) are always extremely small compared to unity, and therefore the Stokes flow problem formulated in Sect. 5.1 is applicable to land ice masses of all shapes and sizes. On the other hand, the applicability of the approximations defined in Sects. 5.2 to 5.4 is limited by the size of the ice masses.作者: defendant 時(shí)間: 2025-3-29 22:15
