標(biāo)題: Titlebook: Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier; Simon Seelig Book 2022 The Editor(s) (if applicab [打印本頁(yè)] 作者: grateful 時(shí)間: 2025-3-21 16:46
書目名稱Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier影響因子(影響力)
書目名稱Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier影響因子(影響力)學(xué)科排名
書目名稱Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier網(wǎng)絡(luò)公開度
書目名稱Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier被引頻次
書目名稱Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier被引頻次學(xué)科排名
書目名稱Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier年度引用
書目名稱Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier年度引用學(xué)科排名
書目名稱Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier讀者反饋
書目名稱Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier讀者反饋學(xué)科排名
作者: MOAN 時(shí)間: 2025-3-21 22:36 作者: conflate 時(shí)間: 2025-3-22 04:21 作者: commute 時(shí)間: 2025-3-22 05:38
2625-3577 Hydraulic properties of the hydrostratigraphic units constituting the rock glacier are estimated and groundwater recharge fluxes quantified. Fundamental proper978-3-658-37072-5978-3-658-37073-2Series ISSN 2625-3577 Series E-ISSN 2625-3615 作者: BARK 時(shí)間: 2025-3-22 10:25 作者: 冷漠 時(shí)間: 2025-3-22 14:29
Discussion,ogical behavior of the Innere ?lgrube are identified by Wagner et al. (in prep.). The integration of a distributed parameter model focusing on dominant processes at the rock glacier scale into this generic framework requires a coordinated evaluation of models characterizing different scales (Grayson and Bl?schl, 2000; Sivapalan et al., 2003).作者: 冷漠 時(shí)間: 2025-3-22 20:58
https://doi.org/10.1007/b138901wnstream rivers and aquifers. The Alpine climate has been subject to significant changes during the last decades and is expected to be affected by the global climate response to increasing greenhouse gas concentrations during the 21. century (Gobiet et al., 2014). River peak runoff is predicted to s作者: escalate 時(shí)間: 2025-3-23 00:57 作者: 慢慢流出 時(shí)間: 2025-3-23 05:25
https://doi.org/10.1007/b138901 data using a multi-disciplinary approach. Evaluation of surface displacement rates within the framework of a simple creep model yields a first approximation of the permafrost thickness distribution in those parts of the rock glacier that are not covered by geophysical measurements. A 3D geometrical作者: 減少 時(shí)間: 2025-3-23 06:09
Konrad Maurer,Nicolas Lang,Joachim Eckert points derived from the geophysical profiles, and 5510 surface displacement vectors distributed across the rock glacier surface. Long-term creep rates are calculated using . = 3, . = 2.4·10. Pa.?s., . = 1604 kg?m., and . = 1826.67 kg?m.. The obtained model consists of a set of four continuous surfa作者: 毀壞 時(shí)間: 2025-3-23 10:52
Praxis der evozierten Potentialeogical behavior of the Innere ?lgrube are identified by Wagner et al. (in prep.). The integration of a distributed parameter model focusing on dominant processes at the rock glacier scale into this generic framework requires a coordinated evaluation of models characterizing different scales (Grayson作者: RALES 時(shí)間: 2025-3-23 16:47
https://doi.org/10.1007/978-3-642-85196-4 reflects site specific characteristics of the rock glacier and its catchment derived from a multi-disciplinary approach, provides a comprehensive basis for a prospective distributed parameter model at the rock glacier scale, and is constrained by a lumped parameter rainfall runoff model characteriz作者: 油膏 時(shí)間: 2025-3-23 18:16
https://doi.org/10.1007/978-3-642-85196-4 basis for a prospective distributed parameter model complementing the lumped-parameter rainfall-runoff model provided by Wagner et al. (in prep.). The specified aquifer geometry and boundary conditions can be easily integrated into a numerical groundwater flow model. The estimated hydraulic propert作者: 冷淡一切 時(shí)間: 2025-3-24 02:05 作者: 錢財(cái) 時(shí)間: 2025-3-24 04:58 作者: Annotate 時(shí)間: 2025-3-24 06:49
Praxis der evozierten Potentialeogical behavior of the Innere ?lgrube are identified by Wagner et al. (in prep.). The integration of a distributed parameter model focusing on dominant processes at the rock glacier scale into this generic framework requires a coordinated evaluation of models characterizing different scales (Grayson and Bl?schl, 2000; Sivapalan et al., 2003).作者: Visual-Field 時(shí)間: 2025-3-24 11:52
https://doi.org/10.1007/978-3-658-37073-2Groundwater flow; Hydraulic properties; Active rock glacier; Conceptual model; Storage capacity; Austria作者: 天空 時(shí)間: 2025-3-24 17:48
978-3-658-37072-5The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Fachmedien Wies作者: covert 時(shí)間: 2025-3-24 23:05 作者: pacifist 時(shí)間: 2025-3-25 00:52 作者: neologism 時(shí)間: 2025-3-25 03:46 作者: innate 時(shí)間: 2025-3-25 11:01
https://doi.org/10.1007/978-3-642-85196-4ing the catchment scale. It complies with the downward approach to hydrological prediction by attempting to explore the dominant processes identified to control the catchment response by Wagner et al.作者: 使厭惡 時(shí)間: 2025-3-25 13:47
2625-3577 nd retarding flood propagation after heavy precipitation events. Progressing climate change alters climatic and meteorological boundary conditions as well as the hydraulic response of alpine catchments by ablating glaciers and thawing permafrost. Rock glaciers exert a controlling influence on the ca作者: 有其法作用 時(shí)間: 2025-3-25 15:49 作者: 音的強(qiáng)弱 時(shí)間: 2025-3-25 21:10
https://doi.org/10.1007/b138901imation of the permafrost thickness distribution in those parts of the rock glacier that are not covered by geophysical measurements. A 3D geometrical model of the internal structure is obtained for the complete rock glacier by combining this approximation with the structures identified by the geophysical survey.作者: Boycott 時(shí)間: 2025-3-26 02:40 作者: Obsessed 時(shí)間: 2025-3-26 05:52 作者: 嚙齒動(dòng)物 時(shí)間: 2025-3-26 09:51 作者: Horizon 時(shí)間: 2025-3-26 12:37
Methods,imation of the permafrost thickness distribution in those parts of the rock glacier that are not covered by geophysical measurements. A 3D geometrical model of the internal structure is obtained for the complete rock glacier by combining this approximation with the structures identified by the geophysical survey.作者: 易彎曲 時(shí)間: 2025-3-26 18:59
Results and Interpretation,s are calculated using . = 3, . = 2.4·10. Pa.?s., . = 1604 kg?m., and . = 1826.67 kg?m.. The obtained model consists of a set of four continuous surfaces which are spatially constrained by the rock glacier boundaries outlined by Wagner et al. (2019a) (fig. 2.3b).作者: 無(wú)意 時(shí)間: 2025-3-26 23:20 作者: fleeting 時(shí)間: 2025-3-27 02:35
Introduction,wnstream rivers and aquifers. The Alpine climate has been subject to significant changes during the last decades and is expected to be affected by the global climate response to increasing greenhouse gas concentrations during the 21. century (Gobiet et al., 2014). River peak runoff is predicted to s作者: 印第安人 時(shí)間: 2025-3-27 07:35 作者: Offensive 時(shí)間: 2025-3-27 12:48 作者: 不連貫 時(shí)間: 2025-3-27 16:29
Results and Interpretation, points derived from the geophysical profiles, and 5510 surface displacement vectors distributed across the rock glacier surface. Long-term creep rates are calculated using . = 3, . = 2.4·10. Pa.?s., . = 1604 kg?m., and . = 1826.67 kg?m.. The obtained model consists of a set of four continuous surfa作者: 不能仁慈 時(shí)間: 2025-3-27 18:18 作者: abreast 時(shí)間: 2025-3-28 01:34 作者: Melodrama 時(shí)間: 2025-3-28 04:21
Outlook, basis for a prospective distributed parameter model complementing the lumped-parameter rainfall-runoff model provided by Wagner et al. (in prep.). The specified aquifer geometry and boundary conditions can be easily integrated into a numerical groundwater flow model. The estimated hydraulic propert作者: 艱苦地移動(dòng) 時(shí)間: 2025-3-28 07:55
10樓作者: watertight, 時(shí)間: 2025-3-28 10:39
10樓作者: 緊張過(guò)度 時(shí)間: 2025-3-28 17:23
10樓作者: 薄膜 時(shí)間: 2025-3-28 20:45
10樓
