標題: Titlebook: Barrier Dynamics and Response to Changing Climate; Laura J. Moore,A. Brad Murray Book 2018 Springer International Publishing AG 2018 Barri [打印本頁] 作者: Enkephalin 時間: 2025-3-21 18:41
書目名稱Barrier Dynamics and Response to Changing Climate影響因子(影響力)
書目名稱Barrier Dynamics and Response to Changing Climate影響因子(影響力)學科排名
書目名稱Barrier Dynamics and Response to Changing Climate網(wǎng)絡公開度
書目名稱Barrier Dynamics and Response to Changing Climate網(wǎng)絡公開度學科排名
書目名稱Barrier Dynamics and Response to Changing Climate被引頻次
書目名稱Barrier Dynamics and Response to Changing Climate被引頻次學科排名
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書目名稱Barrier Dynamics and Response to Changing Climate年度引用學科排名
書目名稱Barrier Dynamics and Response to Changing Climate讀者反饋
書目名稱Barrier Dynamics and Response to Changing Climate讀者反饋學科排名
作者: 冥想后 時間: 2025-3-21 23:24 作者: 大火 時間: 2025-3-22 04:06 作者: 共同時代 時間: 2025-3-22 07:17 作者: CRUC 時間: 2025-3-22 12:15 作者: anus928 時間: 2025-3-22 13:48 作者: CLEAR 時間: 2025-3-22 19:53 作者: 肌肉 時間: 2025-3-22 22:49
Applications in Mathematical Financesea-level rise is accelerating, many barriers islands are urban centers, and barriers buffer mainland shorelines and estuaries from ocean processes, especially during storms. Here, we show that Onslow Beach, NC, a sediment-starved transgressive barrier island located along a cuspate shoreline, had a作者: Indelible 時間: 2025-3-23 02:15 作者: musicologist 時間: 2025-3-23 09:31
Heat Kernel Method and its Applicationsompanies hurricanes and extra-tropical storms. In this respect, the ability of the foredune to recover following a storm determines whether a barrier island can maintain elevation as sea level rises and the island migrates landward through the redistribution of sediment to the back of the island thr作者: 娘娘腔 時間: 2025-3-23 13:14
Heat Kernel and Quantum Gravityelatively simple insights, which facilitate more surprising conclusions as more complicated cases are considered. The simplest case assumes: (1) a constant depth beyond which sediment transport is negligible; (2) a lack of gradients in net long-term alongshore sediment flux that add or remove sedime作者: inspiration 時間: 2025-3-23 17:49
Heat Kernel and Quantum Gravity sediment .. This envelope is contained between the shoreface and underlying surface defined by the continental shelf and coastal plain (i.e., the substrate). Barrier form also depends on coastal change that is constrained, following reasonably well-established principles, by the volume and type of 作者: 心胸開闊 時間: 2025-3-23 22:06 作者: 輕推 時間: 2025-3-24 00:41
Lecture Notes in Physics Monographsarriers will depend on the degree to which these landforms can maintain elevation above sea level while also migrating landward. We are increasingly learning that ecomorphodynamic interactions (i.e., interactions between morphology, fluid dynamics, and/or sediment transport with biological processes作者: 安撫 時間: 2025-3-24 04:08
Heat Kernel and Quantum Gravityents of coastal ecosystems. The shape and growth characteristics of coastal foredunes, typically characterized by simple morphometrics such as dune toe and crest elevations, and dune volume, are a product of both physical and biological forces. By influencing foredune shape, these forces ultimately 作者: Lignans 時間: 2025-3-24 06:50 作者: flimsy 時間: 2025-3-24 13:08 作者: 檢查 時間: 2025-3-24 18:37 作者: 發(fā)芽 時間: 2025-3-24 22:25
Heat Kernel Method and its Applicationsrodynamic models aid in understanding the magnitude of changes, and the impact on barrier morphology. Future changes to coastal systems may be anticipated based upon changes that have occurred in the past.作者: 愚蠢人 時間: 2025-3-24 23:18
Applications in Mathematical Financee island was seaward of its present location and an open-water lagoon separated it from the mainland. Barrier-island transgression progressed mainly through overwash processes and saltmarsh replaced the lagoon by AD 1500. During the nineteenth century, the number and landward extent of washover depo作者: Console 時間: 2025-3-25 06:40
Heat Kernel Method and its Applicationsentennial timescales. Stratigraphic architecture reveals two prominent transgressive surfaces. A lower flooding surface separates red fluvial-deltaic clay from overlying bay mud and an upper erosional surface separates back-barrier deposits from overlying shoreface and foreshore deposits..Radiocarbo作者: 助記 時間: 2025-3-25 10:02
Heat Kernel Method and its Applicationsthe foredune requires that sediment removed to the nearshore during a storm be returned to the beachface through the landward migration and welding of the innermost bars where it is eventually transported to the backshore and trapped by vegetation. Field observations from Padre Island in Texas, Sant作者: 躲債 時間: 2025-3-25 12:20 作者: vascular 時間: 2025-3-25 19:29 作者: Agility 時間: 2025-3-25 22:12 作者: 音樂會 時間: 2025-3-26 03:33
Lecture Notes in Physics Monographs), which is itself a product of couplings between vegetation and sediment transport processes. The cross-shore and alongshore shape of coastal foredunes, in the presence of shoreline erosion or shoreline accretion, is influenced by the distance from the shoreline that vegetation can grow, the rates 作者: configuration 時間: 2025-3-26 05:50
Heat Kernel and Quantum Gravitys suggest that PNW dune shape is primarily a function of sediment supply and the geographic distribution of two species of non-native beach grasses (. and .). Over recent decades, . (American beachgrass) has increased its dominance over . (European beachgrass) on dunes where it was originally plante作者: NOVA 時間: 2025-3-26 10:17
https://doi.org/10.1007/3-540-46523-5ine erosion, and increases to dune height or seawall construction to prevent flooding and damage from overwash during storm events. Over time scales of years to decades, hazard-mitigation actions impact natural, spatio-temporal barrier processes such as washover deposition and planform transgression作者: SPALL 時間: 2025-3-26 13:36 作者: locus-ceruleus 時間: 2025-3-26 18:42
Runaway Barrier Island Transgression Concept: Global Case Studiess and transforms some ebb-dominated channels to flood-dominated channels. This condition leads to sand movement into the back-barrier, which builds and enlarges flood-tidal deltas, filling the newly created accommodation space. The model hypothesizes that sand contributed to the growth of the ebb an作者: legislate 時間: 2025-3-26 23:47
Drowned Barriers as Archives of Coastal-Response to Sea-Level Risereadily be deconstructed as they are not in operation simultaneously, nor present along all coasts. However, it is possible to recognize local conditions that make barriers vulnerable to overstepping. It is shown that barrier retreat through overstepping is enhanced by one or more of the following; 作者: 依法逮捕 時間: 2025-3-27 05:09
Barrier Island and Estuary Co-evolution in Response to Holocene Climate and Sea-Level Change: Pamlicrodynamic models aid in understanding the magnitude of changes, and the impact on barrier morphology. Future changes to coastal systems may be anticipated based upon changes that have occurred in the past.作者: 衰老 時間: 2025-3-27 06:27
Abrupt Increase in Washover Deposition Along a Transgressive Barrier Island During the Late Nineteene island was seaward of its present location and an open-water lagoon separated it from the mainland. Barrier-island transgression progressed mainly through overwash processes and saltmarsh replaced the lagoon by AD 1500. During the nineteenth century, the number and landward extent of washover depo作者: 勤勉 時間: 2025-3-27 10:16
Follets Island: A Case of Unprecedented Change and Transition from Rollover to Subaqueous Shoalsentennial timescales. Stratigraphic architecture reveals two prominent transgressive surfaces. A lower flooding surface separates red fluvial-deltaic clay from overlying bay mud and an upper erosional surface separates back-barrier deposits from overlying shoreface and foreshore deposits..Radiocarbo作者: WAX 時間: 2025-3-27 16:00 作者: conformity 時間: 2025-3-27 19:17
Geometric Constraints on Long-Term Barrier Migration: From Simple to Surprising which active sediment transport occurs). In the next simplest case, substrates composed partly of fine sediment (which is lost to the nearshore system when the substrate is eroded) cause a reduction of the slope of the migration trajectory, because more landward migration is required for each incre作者: GROSS 時間: 2025-3-27 22:47
Shoreface Controls on Barrier Evolution and Shoreline Changetal change. Such shoreface evolution has implications for barrier evolution (and vice versa). In this chapter, we review (1) relations between shoreface and barrier form, (2) limits to knowledge on shoreface behavior and insights from depositional records from which systematic changes over time can 作者: 無動于衷 時間: 2025-3-28 02:56
Morphodynamics of Barrier Response to Sea-Level Rise. Even small perturbations to a barrier system traversing the shelf in dynamic equilibrium can kick-start an oscillating retreat. Looking alongshore, shoreline interconnectivity can have a significant effect on shoreline behavior across both space and time. Overall, our morphodynamic modeling result作者: 演講 時間: 2025-3-28 06:24 作者: 虛度 時間: 2025-3-28 11:06 作者: 爭議的蘋果 時間: 2025-3-28 14:47 作者: 機構 時間: 2025-3-28 20:53 作者: commonsense 時間: 2025-3-28 23:05
Runaway Barrier Island Transgression Concept: Global Case Studiesd deteriorate/drown as back-barrier basins transform to intertidal and subtidal areas. This chapter explores how marshes may succumb to rising sea level and how the loss of wetlands will increase the extent and the overall depth of open water in the back-barrier, causing greater tidal exchange. Here作者: A精確的 時間: 2025-3-29 06:45
Drowned Barriers as Archives of Coastal-Response to Sea-Level Riseed in response to early- to mid-Holocene sea-level rise. These coastal archives, when combined with information on sea-level trends, oceanographic conditions and palaeogeography, are valuable palaeo-evidence that can be used to understand the processes and drivers of coastal change. In this chapter,作者: RLS898 時間: 2025-3-29 08:07 作者: 重疊 時間: 2025-3-29 14:12 作者: Madrigal 時間: 2025-3-29 18:05
Follets Island: A Case of Unprecedented Change and Transition from Rollover to Subaqueous Shoalsrial barrier to subaqueous shoals. This system also allows for an examination of coastal response to accelerated sea-level rise, storms, and sediment supply. The landward shoreline retreat rate during historical time is similar to the landward retreat rate of the bay shoreline, hence its current cla
