Bibliografías temáticas / Vegetated dunes

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Literatura académica sobre el tema "Vegetated dunes"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 13 de febrero de 2022

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Artículos de revistas sobre el tema "Vegetated dunes"

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Gralher, Christine, Nobuhisa Kobayashi, and Kideok Do. "WAVE OVERWASH OF VEGETATED DUNES." Coastal Engineering Proceedings 1, no. 33 (2012): 34. http://dx.doi.org/10.9753/icce.v33.sediment.34.

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Sand dunes play a significant role during coastal storms by absorbing the impacts of storm surge and high waves. Therefore, rapid profile changes and destruction of sand dunes, which may be caused by wave-induced overwash, lead to an increased flood risk landward of dunes. The effects of vegetation on dune erosion and overwash during storm events, however, have never been studied. This study is based on a laboratory experiment investigating the effects of woody plants on dune erosion and overwash of high and low dunes. During the five tests conducted foredune scarping was observed for the thre
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2

McCann, S. B., and M. L. Byrne. "Stratification models for vegetated coastal dunes in Atlantic Canada." Proceedings of the Royal Society of Edinburgh. Section B. Biological Sciences 96 (1989): 203–15. http://dx.doi.org/10.1017/s0269727000010939.

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SynopsisThe principal types of stratification and some characteristic sedimentary sequences found in vegetated coastal dunes in Atlantic Canada are described. Four examples are selected to show a range of dune types and depositional settings. In each case the documentation and interpretation of the internal structure and stratification has made an important contribution to understanding the evolution of the dunes. Stratification and depositional models are presented for:(1) a single, continuous, transgressive foredune ridge which maintains its form during transgression;(2) a discontinuous tran
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Tsoar, H. "Linear dunes - forms and formation." Progress in Physical Geography: Earth and Environment 13, no. 4 (1989): 507–28. http://dx.doi.org/10.1177/030913338901300402.

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Most geomorphologists and geologists do not differentiate the various types of linear dune and refer to them as one dune type mainly in the terms of linear, longitudinal or seif dunes. In recent morphodynamic and genetic classifications of dunes, all types of linear dunes are lumped under the heading of longitudinal dunes (Wasson and Hyde, 1983; Hunter et al., 1983). This review, however, substantiates three different simple linear dunes - lee dunes, seifs and vegetated- linear - each of which has a different shape and mechanism of formation and elongation.
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McArthur, E., and Stewart Sanderson. "Great Sand Dunes National Monument Vegetation Patterns." UW National Parks Service Research Station Annual Reports 15 (January 1, 1991): 185–89. http://dx.doi.org/10.13001/uwnpsrc.1991.3019.

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This project is designed to chacterize and map the vegetation of the Great Sand Dunes National Monument, Colorado (GSDNM) and to determine if the vegetated areas in the dune field are permanent, temporary, or migratory. It is not known if the vegetation around the dunes is encroaching on the dunes, being replaced by the dunes or is stable. There are also concerns about the possible effect a proposed water export project adjacent to GSDNM would have on the dunes and their vegetation.
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5

Goldsmith, Victor. "Coastal sand dunes as geomorphological systems." Proceedings of the Royal Society of Edinburgh. Section B. Biological Sciences 96 (1989): 3–15. http://dx.doi.org/10.1017/s0269727000010824.

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SynopsisThe importance of aeolian deposition is clearly shown by the size and bulk of coastal dunes. Sand dunes occur where there is a large supply of sand, a wind to move it, and a place in which it can accumulate. A dune classification is presented which takes into account the origin, internal geometry and surface geomorphology of coastal dunes. Since the main element that distinguishes coastal dunes from desert dunes is vegetation, the relative amount of vegetation may be used as a typology. Four dune types are distinguished: vegetated dunes, parabolic dunes, medanos (i.e. large sand hills
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6

Figlus, Jens, Jacob M. Sigren, Anna R. Armitage, and Robert C. Tyler. "EROSION OF VEGETATED COASTAL DUNES." Coastal Engineering Proceedings 1, no. 34 (2014): 20. http://dx.doi.org/10.9753/icce.v34.sediment.20.

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Kortenhaus, Andreas, David Schürenkamp, Thorsten Piontkowitz, and Hocine Oumeraci. "RELIABILITY ASSESSMENT OF A COASTAL DIKE AND DUNE SYSTEM AT THE SOUTH OF FALSTER, DENMARK." Coastal Engineering Proceedings 1, no. 33 (2012): 59. http://dx.doi.org/10.9753/icce.v33.management.59.

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The ‘Falster dike’ is a system of a coastal vegetated dunes with a grass-covered sand dike protecting a low-lying area of about 7,000 summer houses, many of which being inhabited during winter, and therefore in danger of any storm surge induced flooding. The paper discusses (i) the assessment and uncertainties of relevant data such as bathymetry, topography, wind and wave data, water levels; (ii) deterministic calculations of wave run-up and overtopping of the dike without dunes; (iii) the calculations of dune erosion; and (iv) a reliability assessment of a dune and dike system. Results sugges
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8

Wilson, BA, NM White, A. Hanley, and DL Tidey. "Population fluctuations of the New Holland mouse Pseudomys novaehollandiae at Wilson?s Promontory National Park, Victoria." Australian Mammalogy 27, no. 1 (2005): 49. http://dx.doi.org/10.1071/am05049.

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The New Holland mouse (Pseudomys novaehollandiae) was first recorded at Wilson?s Promontory in 1972 in heathland vegetation, but has not been located in this habitat subsequently. The species was not trapped again until 1993 when it was found in calcarenite dune woodland on the Yanakie Isthmus. The aims of this study were to assess the population dynamics and habitat use of the species in this dune habitat. Mark-recapture trapping was conducted at three sites from 1999 to 2002. One site was located on low (0 - 5 m), flat sand dunes and open swales, another on medium (5 ? 10 m) vegetated dunes,
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Mahmoud, Ahmed Mutasim Abdalla, Alessandro Novellino, Ekbal Hussain, Stuart Marsh, Panagiotis Psimoulis, and Martin Smith. "The Use of SAR Offset Tracking for Detecting Sand Dune Movement in Sudan." Remote Sensing 12, no. 20 (2020): 3410. http://dx.doi.org/10.3390/rs12203410.

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Sand movement is one of the main environmental hazards in Northern Sudan that threaten livelihood and rural communities. This paper investigates for the first time the use of the Synthetic Aperture Radar (SAR) offset tracking technique for detecting sand movement in Northern Sudan, and distinguishes the impact of the movement influencing factors: wind speed/direction, vegetation and topography. High-resolution images from the Sentinel-1 satellite were used for the generation of displacement maps. Three different dune fields with different characteristics were investigated for a study period be
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10

Smyth, Thomas AG, Irene Delgado-Fernandez, Derek WT Jackson, Brian Yurk, and Paul Rooney. "Greedy parabolics: Wind flow direction within the deflation basin of parabolic dunes is governed by deflation basin width and depth." Progress in Physical Geography: Earth and Environment 44, no. 5 (2020): 643–60. http://dx.doi.org/10.1177/0309133319899306.

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Parabolic dunes are ‘U’ or ‘V’-shaped aeolian landforms that form on pre-existing sand deposits. Their morphology consists of an upwind deflation basin, bordered by often vegetated trailing arms and a downwind depositional lobe. The orientation of parabolic dunes is commonly attributed to the prevailing or resultant wind direction. Consequently, the orientation of parabolic dunes stabilised by vegetation growth has been used as a proxy for wind direction during past climates in several studies. However, the ability or extent of parabolic dune morphology to steer incident wind flow parallel to
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Tesis sobre el tema "Vegetated dunes"

1

Durán, Orencio. "Vegetated dunes and barchan dune fields." [S.l. : s.n.], 2006. http://nbn-resolving.de/urn:nbn:de:bsz:93-opus-29639.

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Malta, J?lia Varella. "Experimento de fluxo de sedimentos em um segmento de campo de dunas e?licas costeiras de Jenipabu - Litoral oriental do Rio Grande do Norte." Universidade Federal do Rio Grande do Norte, 2012. http://repositorio.ufrn.br:8080/jspui/handle/123456789/18831.

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Made available in DSpace on 2015-03-13T17:08:35Z (GMT). No. of bitstreams: 1 JuliaVM_DISSERT.pdf: 4236567 bytes, checksum: be73f658e3777fffb5d25f1a4d23b8d3 (MD5) Previous issue date: 2012-09-06<br>Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior<br>This study analyzed measurements of the aeolian transport using vertical sand traps across the field dunes of Jenipabu, in the municipality of Extremoz, Rio Grande do Norte state to the North of Natal city. These measurements were used as parameters for the sand aeolian transport in the region. Before the field trips a map of landscape
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3

Durán, Orencio [Verfasser]. "Vegetated dunes and barchan dune fields / vorgelegt von Orencio Durán." 2007. http://d-nb.info/983771642/34.

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Libros sobre el tema "Vegetated dunes"

1

Joop, Mourik, ed. Hiëroglyfen van het zand: Vegetatie en landschap van de Amsterdamse Waterleidingduinen. Gemeentewaterleidingen Amsterdam, 1999.

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2

Houston, John. The conservation and management of coastal vegetated shingle in England: Report of the meeting at Salthouse, North Norfolk on 18th September 2008 : organised by the Sand Dune and Shingle Network on behalf of Natural England : report. Liverpool Hope University Press, 2009.

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Capítulos de libros sobre el tema "Vegetated dunes"

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Doody, J. Patrick. "Vegetated States and Values – Inland Dune." In Sand Dune Conservation, Management and Restoration. Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-4731-9_5.

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Doody, J. Patrick. "Trends and Trade-offs – Inland Vegetated Dune." In Sand Dune Conservation, Management and Restoration. Springer Netherlands, 2012. http://dx.doi.org/10.1007/978-94-007-4731-9_7.

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3

Bristow, C. S., B. G. Jones, G. C. Nanson, C. Hollands, M. Coleman, and D. M. Price. "GPR surveys of vegetated linear dune stratigraphy in central Australia: Evidence for linear dune extension with vertical and lateral accretion." In Special Paper 432: Stratigraphic Analyses Using GPR. Geological Society of America, 2007. http://dx.doi.org/10.1130/2007.2432(02).

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Informes sobre el tema "Vegetated dunes"

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Bryant, Duncan, Mary Bryant, Jeremy Sharp, Gary Bell, and Christine Moore. The Response of Vegetated Dunes to Wave Attack. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/41580.

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Vegetation is believed to increase the stability of dunes during wave attack, but limited data is available. A physical model study was performed to evaluate changes in the dune stability with and without biomass, both above and belowground. The above and belowground biomass was modeled using wooden dowels and coir fibers, respectively. For both the collision and overwash storm impact regimes, the results of this study clearly demonstrate that the inclusion of biomass in the model dune reduces the erosion and overwash. The combination of both above and belowground biomass was the most effectiv
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2

Conery, Ian, Nicholas Cohn, Nicholas Spore, and Katherine Brodie. Evaluating Collection Parameters for Mobile Lidar Surveys in Vegetated Beach-Dune Settings. Engineer Research and Development Center (U.S.), 2020. http://dx.doi.org/10.21079/11681/37759.

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Map showing a vegetated dune field in Central Alaska. US Geological Survey, 1985. http://dx.doi.org/10.3133/mf1708.

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