標題: Titlebook: Base-level Impact; A Geomorphic Approac Dan Bowman Book 2023 The Editor(s) (if applicable) and The Author(s), under exclusive license to Sp [打印本頁] 作者: HBA1C 時間: 2025-3-21 17:57
書目名稱Base-level Impact影響因子(影響力)
書目名稱Base-level Impact影響因子(影響力)學科排名
書目名稱Base-level Impact網(wǎng)絡公開度
書目名稱Base-level Impact網(wǎng)絡公開度學科排名
書目名稱Base-level Impact被引頻次
書目名稱Base-level Impact被引頻次學科排名
書目名稱Base-level Impact年度引用
書目名稱Base-level Impact年度引用學科排名
書目名稱Base-level Impact讀者反饋
書目名稱Base-level Impact讀者反饋學科排名
作者: 可能性 時間: 2025-3-21 21:29 作者: JECT 時間: 2025-3-22 04:06
Dan BowmanPresents principles and conclusions gained by field work, by laboratory studies, and by models.Examines wide literature in fluvial geomorphology.Examines different types of base- levels, their altitud作者: 吝嗇性 時間: 2025-3-22 07:55 作者: Vertical 時間: 2025-3-22 12:30
Casta?eda’S Philosophy of Languagee-level, ?120 to ?130?m below the present sea level. The rising global sea level to its recent level realized at 18–6?ka. Lakes or playas in the continental interiors compose a different base-level category. Resistant outcrops or waterfalls are local base-levels which have always an ultimate base-le作者: 客觀 時間: 2025-3-22 13:39 作者: Conflagration 時間: 2025-3-22 20:43 作者: 廢除 時間: 2025-3-22 22:41
https://doi.org/10.1007/978-3-658-17872-7adually be transmitted upstream. The balance between sediment supply and sediment transport efficiency determines the response of the channel to base-level perturbations. Bedrock erosion is proportional to the stream energy available and depends on the channel slope and discharge and inversely propo作者: 帽子 時間: 2025-3-23 02:17 作者: Intuitive 時間: 2025-3-23 07:35
https://doi.org/10.1007/978-3-322-81765-5es the erosion efficiency. Knickpoints propagate upstream at a rate characterized by the power law function of the upstream drainage area. 2. The . affects the erodibility and includes the dip and its orientation, jointing and layering or massiveness. 3. The . which provide an incision tool and migh作者: ARK 時間: 2025-3-23 10:21 作者: RAG 時間: 2025-3-23 16:03 作者: 漂亮才會豪華 時間: 2025-3-23 18:36
Richard D. F. Harris,Murat Mazibas approximate a smooth, concave-upward continuous curve that has been claimed to be a necessary marker for steady state. Graded profiles are controlled by a long-term balance between sediment supply and sediment transport capacity. Steep channels at the upslope end of drainage basins develop self‐enh作者: 高興去去 時間: 2025-3-24 01:14
Hedge Funds and Financial Marketsrrowest incised valleys are formed when base-level fall is notably rapid. Increased precipitation accounts for increase in discharge, corresponding to an assumed increase in the erosional efficiency. Maximum incision rates occur at moderate sediment supply rates relative to the sediment transport ca作者: placebo-effect 時間: 2025-3-24 05:31
Hedge Funds and Financial MarketsGibraltar arc and global sea level changes. The consequent rapid and huge Mediterranean base-level drop of about 1500?m triggered an extensive subaerael erosion along the exposed Mediterranean margins, thereby demonstrating a dramatic base-level impact. The Messinian base-level fall initiated deep i作者: 格子架 時間: 2025-3-24 06:46
Bilanzierung und Bewertung von Mikro-Hedgesalling base-level has not yet been transmitted. This makes a typical . based on differences in gradients, incision rates, cross-sectional morphology, in the abundance of terraces as well as in slope dynamics. A river terrace designates a low base-level that has initiated an upstream propagating wave作者: EVEN 時間: 2025-3-24 11:56 作者: 騙子 時間: 2025-3-24 16:39
https://doi.org/10.1007/978-3-322-83460-7oint at the tributary junction, i.e., at the confluence of the tributary with the main stem. Tributaries adjust to the mainstream as to a local base-level and are directly?uncontrolled by the terminal base-level downstream. Tributary junctions may steepen and become a knickpoint which separates the 作者: Amendment 時間: 2025-3-24 22:49 作者: 失敗主義者 時間: 2025-3-25 02:21
Von Alfred W. Jones zur Hedgefonds-Industrientervals, high-intensity short rain events, limited-area rain cells and ephemeral streams with flash floods of peaky hydrographs. High flow velocities attain 4–6?m/s along typically steep (>?1°) channels in an area dominated by soft erodible sediments. Lake Lisan, the Late-Pleistocene precursor of t作者: STEER 時間: 2025-3-25 06:13 作者: Immunotherapy 時間: 2025-3-25 07:28 作者: 牢騷 時間: 2025-3-25 14:31 作者: certitude 時間: 2025-3-25 18:03 作者: 書法 時間: 2025-3-25 20:45
Von Alfred W. Jones zur Hedgefonds-Industriese-level drop. The typical divergence of river terraces downstream and the convexity of the channel profiles as well as their steepness are controlled in the Dead Sea area by the accelerating base-level fall and the control of the steep clinoform structure of the fan deltas. The gap between the recu作者: Mingle 時間: 2025-3-26 00:10
Controlling Factors,the river would normally adjust at grade. 6. The . of the base-level change. In case base-level lowering is small, the channel may adjust only by increased sinuosity. The longer the duration of a base-level fall, the more adjustments of the fluvial system can be expected. Because of different backgr作者: 菊花 時間: 2025-3-26 04:26
Morphological Products,ree dimensional envelope of aggradation and degradation history including repeated cut-and-fill cycles. Coupling between incising channels and hillslopes plays an important role in the relief evolution. Quantifying landslides shows that the frequency of slope failures per unit area is largest in zon作者: 諂媚于性 時間: 2025-3-26 09:10
Small-Scale Networks and Man-Made Structures,el bed is a man-made lowered? local base-level. On its upstream end, incision typically evolves as?a? retreating knickpoint. Dewatering reservoirs means their conversion from a sediment sink to a sediment source. The magnitude and rate of reservoir sediment erosion, following dam removal, starts ini作者: violate 時間: 2025-3-26 13:42
The Dead Sea Area as a Field Laboratory,se-level drop. The typical divergence of river terraces downstream and the convexity of the channel profiles as well as their steepness are controlled in the Dead Sea area by the accelerating base-level fall and the control of the steep clinoform structure of the fan deltas. The gap between the recu作者: CERE 時間: 2025-3-26 19:43
models, based on the widely scattered literature. The chapters include presentation of different types of base-levels, discussing the constraints of their altitude, the degradation and aggradation responses, t978-3-031-24996-9978-3-031-24994-5作者: 雕鏤 時間: 2025-3-26 23:28
Hedge Fonds, Banken und Finanzkrisen,ures upstream. The greater the drainage area and the higher the rate of the base-level fall, the shorter is the expected delay. Additional competing controls that determine the rate of knickpoint retreat include the stream gradient, weathering processes, abrasion and undermining.作者: amenity 時間: 2025-3-27 01:17
Richard D. F. Harris,Murat Mazibasithologic boundaries, longitudinal profiles may become completely unrelated to the base-level impact. The profiles always adjust to the first adjacent downstream local base-level, not to the ultimate one.作者: 徹底檢查 時間: 2025-3-27 08:45 作者: 發(fā)怨言 時間: 2025-3-27 10:54 作者: freight 時間: 2025-3-27 13:38
Longitudinal Profiles,ithologic boundaries, longitudinal profiles may become completely unrelated to the base-level impact. The profiles always adjust to the first adjacent downstream local base-level, not to the ultimate one.作者: 厚顏無恥 時間: 2025-3-27 20:09
The Transient-Equilibrium Test,arks disequilibrium and has yet to adjust to the base-level and to the other controlling conditions. Being in a transient state means that the channel is neither in energy equilibrium nor in a topographic steady state, but is?progressing toward it.作者: 詞匯記憶方法 時間: 2025-3-28 00:53 作者: Finasteride 時間: 2025-3-28 05:24
https://doi.org/10.1007/978-3-322-83460-7main trunk stream from the often “hanging” conditions of the tributary valley. Hanging conditions limit the connectivity and impede upstream transmission of incision signals and thus delay reaching?full equilibrium of the drainage network.作者: 調(diào)色板 時間: 2025-3-28 07:26
Hallesche Schriften zur Betriebswirtschaftt or slow relative to the base-level, or subsiding (Vail et al..). Mountain relief is finally controlled by the interplay between rising or falling relief. Eustatic fluctuations of lake levels will cause an increase or decrease in the accommodation space and are usually more frequent than tectonically driven base-level fluctuations.作者: RACE 時間: 2025-3-28 11:07 作者: 改良 時間: 2025-3-28 17:01
Hedge Funds and Financial Markets of mm?year., whereas a very fast rate may reach up to a few m/y. Fluctuation rates of base-levels controlled by tectonics are spread beyond the frequent <1–15 mm?year. range, reaching 100 mm??year. and beyond.作者: 無所不知 時間: 2025-3-28 20:29 作者: ADAGE 時間: 2025-3-29 02:16 作者: browbeat 時間: 2025-3-29 06:41 作者: Presbyopia 時間: 2025-3-29 07:54 作者: syncope 時間: 2025-3-29 11:40
The Messinian Event,xamples for such deep incised paleovallies that propagated far inland, up to several hundreds km. Additional markers of the huge phase of the subaerial erosion following the Messinian base-level drawdown include erosional discordances, submarine scarps, submarine canyons and platforms, mesa-like relief and valley terraces.作者: circuit 時間: 2025-3-29 19:00
Book 2023g the global relief by? processes of erosion and aggradation. In the populated world, entrenchments triggered by base-level changes may become devastating events, damaging agricultural lands, undercutting bridges and destroying roads..The aim of this book, as a chapter in fluviomorphology, is to pre作者: 抗生素 時間: 2025-3-29 23:48
,Discontinuity in Slope—Knickpoints and Knickzones,ickzone is an oversteepened channel reach, often including rapids or pools, that is typically up to a few kms long. Nickzones, as knickpoints, are often transient features, eroding and migrating upstream with time as a response to a base-level fall.作者: 廣口瓶 時間: 2025-3-30 02:43
Tributary Junctions,main trunk stream from the often “hanging” conditions of the tributary valley. Hanging conditions limit the connectivity and impede upstream transmission of incision signals and thus delay reaching?full equilibrium of the drainage network.作者: 浮雕 時間: 2025-3-30 07:17
logy.Examines different types of base- levels, their altitud.Much of the final shaping of the global landscape is accomplished by incision of river networks. The base-level is a principle determinate controlling the global relief by? processes of erosion and aggradation. In the populated world, entr作者: lethargy 時間: 2025-3-30 08:40
Casta?eda’S Philosophy of Languagenental interiors compose a different base-level category. Resistant outcrops or waterfalls are local base-levels which have always an ultimate base-level downstream. The base-level functions as an external forcing on the drainage system and controls its erosive energy.作者: 2否定 時間: 2025-3-30 16:08
https://doi.org/10.1007/978-3-658-17872-7her far up compared to the spatial limited impact of aggradation by a rising base-level. High sediment supply from rivers can restrain a river mouth from being entrenched when base-level falls and may enable, under base-level rise, continued sediment fill basinward.作者: BUDGE 時間: 2025-3-30 18:34 作者: Ingrained 時間: 2025-3-30 21:15
,Base-Level—Definitions and Location,nental interiors compose a different base-level category. Resistant outcrops or waterfalls are local base-levels which have always an ultimate base-level downstream. The base-level functions as an external forcing on the drainage system and controls its erosive energy.
