標(biāo)題: Titlebook: Geomorphology of Proglacial Systems; Landform and Sedimen Tobias Heckmann,David Morche Book 2019 Springer Nature Switzerland AG 2019 Alpine [打印本頁] 作者: 轉(zhuǎn)變 時(shí)間: 2025-3-21 19:42
書目名稱Geomorphology of Proglacial Systems影響因子(影響力)
書目名稱Geomorphology of Proglacial Systems影響因子(影響力)學(xué)科排名
書目名稱Geomorphology of Proglacial Systems網(wǎng)絡(luò)公開度
書目名稱Geomorphology of Proglacial Systems網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Geomorphology of Proglacial Systems被引頻次
書目名稱Geomorphology of Proglacial Systems被引頻次學(xué)科排名
書目名稱Geomorphology of Proglacial Systems年度引用
書目名稱Geomorphology of Proglacial Systems年度引用學(xué)科排名
書目名稱Geomorphology of Proglacial Systems讀者反饋
書目名稱Geomorphology of Proglacial Systems讀者反饋學(xué)科排名
作者: meditation 時(shí)間: 2025-3-21 20:50 作者: indices 時(shí)間: 2025-3-22 03:00 作者: famine 時(shí)間: 2025-3-22 05:41
Rockfall at Proglacial Rockwalls—A Case Study from the Kaunertal, Austriad- and high-magnitude rockfalls with volumes between 100 and 30,000?m. were released between 2006 and 2012. Their scars are clustered in the proglacial high-altitude parts of the Kaunertal. As well, rockwall activity was concentrated in the autumn and winter months.作者: absolve 時(shí)間: 2025-3-22 12:44 作者: MAOIS 時(shí)間: 2025-3-22 14:40 作者: MAOIS 時(shí)間: 2025-3-22 20:49 作者: Digest 時(shí)間: 2025-3-23 00:37 作者: conifer 時(shí)間: 2025-3-23 04:43
5 Auslegung von Netzen im Normalbetrieb,erial origins from the catchment above and the bedrock below the glacier and appears at the glacier surface in the ablation zone. It often forms medial moraines in the upper areas which increase down glacier until the glacier is covered across its full width. Debris-covered glaciers are located in a作者: 鉤針織物 時(shí)間: 2025-3-23 08:40
Klaus Heuck,Klaus-Dieter Dettmanneodetic methods were applied. Specifically, ice surface lowering measured at ablation stakes determined mass loss at the glacier surface, ice surface velocity was measured directly at the same stakes with differential GPS, and geodetic radar and vibroseismic soundings came into operation to investig作者: ENNUI 時(shí)間: 2025-3-23 11:03 作者: gimmick 時(shí)間: 2025-3-23 15:58 作者: CLOUT 時(shí)間: 2025-3-23 19:49
https://doi.org/10.1007/978-3-540-69440-3 the dynamics and hazards of high alpine and proglacial areas. This chapter highlights the state of knowledge in the context of proglacial environments and reviews methods of investigating rock slope failure activity and causes. An alignment of extreme conditions and dynamic processes renders progla作者: 生氣地 時(shí)間: 2025-3-23 22:40
Elektrische Energieversorgung 1ted rockwalls. At the Gepatschferner, Kaunertal (Austria), rockfall activity has been quantified for the past several years using rockfall collector nets, ‘natural’ rockfall traps and multi-temporal LiDAR. Toppling and sliding activity of large unstable rock blocks, considered as precursors of rockf作者: contradict 時(shí)間: 2025-3-24 03:26
https://doi.org/10.1007/978-3-662-06958-5lux of sediments through the proglacial zone represents an increasingly important area for contemporary geomorphological and sedimentological study. The term ‘paraglacial’ is used to describe this heightened geomorphological activity, and the general model of paraglacial basin sediment yield is one 作者: concentrate 時(shí)間: 2025-3-24 06:49
https://doi.org/10.1007/978-3-319-94184-4Alpine Landscapes; Deglaciated Alpine Landscapes; Geomorphology of Proglacial Systems; Proglacial Syste作者: CAMEO 時(shí)間: 2025-3-24 11:04
Tobias Heckmann,David MorchePresents case studies of alpine proglacial systems.Up-to-date overview of the research in alpine environments.Serves as an interesting reference book to geomorphologists, geologists, glaciologists and作者: 昏睡中 時(shí)間: 2025-3-24 18:46 作者: PRISE 時(shí)間: 2025-3-24 20:20 作者: jovial 時(shí)間: 2025-3-25 00:27 作者: 盟軍 時(shí)間: 2025-3-25 04:24 作者: 健談 時(shí)間: 2025-3-25 08:16 作者: maroon 時(shí)間: 2025-3-25 13:32
Auslegung von Netzen im Normalbetrieb,erns. Switzerland has by far the highest proportion of very small (<0.5?km.) proglacial systems. Patagonia has the most even distribution of proglacial systems in terms of areal size and elevation above sea level. We found no east–west or north–south spatial pattern in geometric or topographical met作者: 使入迷 時(shí)間: 2025-3-25 16:12 作者: deface 時(shí)間: 2025-3-25 22:54 作者: Vertebra 時(shí)間: 2025-3-26 01:51
Aufbau von Energieversorgungsnetzen,glacio-fluvial processes, low-temperature conditions, as well as the occurrence of ground ice, are the most effective drivers for geomorphic dynamics and related landform evolution in these proglacial areas. A deeper knowledge of ongoing processes as well as of the amounts of sediment and ground ice作者: 殘廢的火焰 時(shí)間: 2025-3-26 08:17
https://doi.org/10.1007/978-3-662-06956-1ributary valley to the Upper Kaunertal. Results show a diverse genesis and development of different rock glacier parts and lobes, which are mainly related to glacial advances during the Egesen and LIA stadials. More recent developments are largely dependent on (i) sediment sources and pathways const作者: saturated-fat 時(shí)間: 2025-3-26 10:33
https://doi.org/10.1007/978-3-540-69440-3: (i) fracture growth and seismicity arising from the unloading of glacial loads over millennial timescales, and (ii) rock fracture growth and loss of strength as a result of hydrological and thermal effects that fluctuate over daily to seasonal timescales, but are superimposed upon long-term trends作者: dura-mater 時(shí)間: 2025-3-26 12:54 作者: PLE 時(shí)間: 2025-3-26 16:53 作者: Offbeat 時(shí)間: 2025-3-26 22:03 作者: 我說不重要 時(shí)間: 2025-3-27 01:43 作者: aplomb 時(shí)間: 2025-3-27 06:40
Debris-Covered Glacierslacier mass balance as they are regions of significantly enhanced ice melt. The glacier snouts of debris-covered glaciers are often very slow or stagnant, and the terminus positions are stable over long periods. In this case, only small amounts of debris are transported from the glacial into the pro作者: 共棲 時(shí)間: 2025-3-27 12:31
Closing the Balances of Ice, Water and Sediment Fluxes Through the Terminus of Gepatschfernerce, water and sediments entering the narrow terminus at an elevation of 2875?m and leaving it at the glacier snout at 2200?m was based on glacier motion, surface and basal melt rates and on the lateral mass transport to the glacier from rock face and moraine bedrock erosion recorded from repeated te作者: 伴隨而來 時(shí)間: 2025-3-27 16:36
(Ground) Ice in the Proglacial Zoneglacio-fluvial processes, low-temperature conditions, as well as the occurrence of ground ice, are the most effective drivers for geomorphic dynamics and related landform evolution in these proglacial areas. A deeper knowledge of ongoing processes as well as of the amounts of sediment and ground ice作者: Arresting 時(shí)間: 2025-3-27 21:26 作者: 富饒 時(shí)間: 2025-3-27 23:24
Rock Slope Instability in the Proglacial Zone: State of the Art: (i) fracture growth and seismicity arising from the unloading of glacial loads over millennial timescales, and (ii) rock fracture growth and loss of strength as a result of hydrological and thermal effects that fluctuate over daily to seasonal timescales, but are superimposed upon long-term trends作者: 極小量 時(shí)間: 2025-3-28 03:38
Glacial Sediment Stores and Their Reworkingtic complexity and geomorphological evidence of sediment reworking, in the form of deep gullies and associated debris cones and fans, would suggest that such units can yield sediments dependant on multiple climatic, geomorphical and biogeomorphical factors. Similarly, the extent to which the general作者: 600 時(shí)間: 2025-3-28 07:32 作者: engrave 時(shí)間: 2025-3-28 12:30
Glacier Changes Since the Little Ice AgeIce Age (LIA). During this period, the lateral accumulation of rock and debris created impressive moraine walls. Between these LIA moraines and the actual terminus position is the glacier forefield, which is growing as glaciers retreat. Whereas the forefields are constantly changing (e.g. due to the作者: mitten 時(shí)間: 2025-3-28 18:05
An Inventory of Proglacial Systems in Austria, Switzerland and Across Patagoniaely important as sediment sources. Indeed sediment yields from proglacial rivers are amongst the highest measured anywhere in the World. Motivated by a desire to understand where exactly within catchments this sediment is coming from and how it might evolve, this chapter presents the first digital i作者: 破譯密碼 時(shí)間: 2025-3-28 21:40 作者: 拾落穗 時(shí)間: 2025-3-29 02:43 作者: 一再遛 時(shí)間: 2025-3-29 06:26 作者: 支柱 時(shí)間: 2025-3-29 07:13 作者: 的闡明 時(shí)間: 2025-3-29 14:43
Rock Slope Instability in the Proglacial Zone: State of the Art the dynamics and hazards of high alpine and proglacial areas. This chapter highlights the state of knowledge in the context of proglacial environments and reviews methods of investigating rock slope failure activity and causes. An alignment of extreme conditions and dynamic processes renders progla
