Relevant bibliographies by topics / Coastal foredune

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Book chapters
  4. Conference papers
  5. Reports

Academic literature on the topic 'Coastal foredune'

Author: Grafiati
Published: 14 March 2023
Last updated: 31 July 2025

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Journal articles on the topic "Coastal foredune"

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Zarnetske, Phoebe L., Peter Ruggiero, Eric W. Seabloom, and Sally D. Hacker. "Coastal foredune evolution: the relative influence of vegetation and sand supply in the US Pacific Northwest." Journal of The Royal Society Interface 12, no. 106 (2015): 20150017. http://dx.doi.org/10.1098/rsif.2015.0017.

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Biophysical feedbacks between vegetation and sediment are important for forming and modifying landscape features and their ecosystem services. These feedbacks are especially important where landscape features differ in their provision of ecosystem services. For example, the shape of coastal foredunes, a product of both physical and biological forces, determines their ability to protect communities from rising seas and changing patterns of storminess. Here we assessed how sand supply and changes in vegetation over interannual (3 year) and decadal (21 year) scales influenced foredune shape along
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Schweiger, Constantin, Björn Mehrtens, Thea Bölker, et al. "NUMERICAL STUDY ON THE INFLUENCE OF COASTAL FOREDUNES ON STORM- INDUCED EROSION." Coastal Engineering Proceedings, no. 38 (May 29, 2025): 35. https://doi.org/10.9753/icce.v38.sediment.35.

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In the context of nature-based solutions, there is a growing interest in considering the benefits of ecosystem services towards sustainable coastal protection measures (Sutton- Grier et al. 2015). Coastal dunes serve as a natural barrier at sandy coastlines. While higher elevated dunes protect the adjacent hinterland from flooding during severe storm surges (e.g. Figlus 2022), coastal foredunes can act as a first buffer zone during storm surges by enhancing near- shore wave breaking-induced energy dissipation as a result of the deposition of eroded sand in the foreshore bathymetry (Temmerman e
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Donker, Jasper, Marcel van Maarseveen, and Gerben Ruessink. "Spatio-Temporal Variations in Foredune Dynamics Determined with Mobile Laser Scanning." Journal of Marine Science and Engineering 6, no. 4 (2018): 126. http://dx.doi.org/10.3390/jmse6040126.

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Coastal foredunes are highly dynamic landforms because of rapid erosion by waves and currents during storm surges in combination with gradual accretion by aeolian transport during more quiescent conditions. While our knowledge into the mechanisms behind foredune erosion have reached considerable maturity, this is not the case for foredune growth. High resolution spatio-temporal data sets of beach and foredune topography, which are needed to increase our understanding of mechanisms behind aeolian transport in coastal environments and to develop predictive dune-accretion models, are scarce. Here
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Pickart, Andrea J. "Ammophila Invasion Ecology and Dune Restoration on the West Coast of North America." Diversity 13, no. 12 (2021): 629. http://dx.doi.org/10.3390/d13120629.

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The invasive ecosystem engineer Ammophila arenaria, native to Europe, was first introduced to California (USA) in 1896. More than a century later, it has come to dominate coastal foredune vegetation on the west coast of North America to the near exclusion of native species. A. arenaria builds a narrow, steep, peaked, and densely vegetated foredune, in contrast to the broad, more sparsely vegetated foredunes built by the native Elymus mollis. As such, it has modified dune processes by fixing the foredune and disrupting exchange of sediment between the beach, foredune, and dunefield. In the 1930
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Psuty, Norbert P. "An application of science to the management of coastal dunes along the Atlantic coast of the U.S.A." Proceedings of the Royal Society of Edinburgh. Section B. Biological Sciences 96 (1989): 289–307. http://dx.doi.org/10.1017/s0269727000010988.

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SynopsisCoastal foredune management begins with an understanding of and appreciation for the dynamics of dune creation, development and decay. Sediment exchange between the dune and beach components of the total dune–beach profile is a necessary element in foredune creation and development. Foredune development is enhanced by a slightly negative total dune–beach budget. Foredune crestlines display alongshore periodicities in displacement that are related to beach processes. Effective management is based on the dimensions of the alongshore foredune variations and the retention of sediment in th
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Davidson, Samuel G., Patrick A. Hesp, and Graziela Miot da Silva. "Controls on dune scarping." Progress in Physical Geography: Earth and Environment 44, no. 6 (2020): 923–47. http://dx.doi.org/10.1177/0309133320932880.

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The controls that affect the degree of spatio-temporal change to foredunes following scarping are reviewed herein. As sea-levels rises and climate changes, dune scarping will become more common. Thus, it is critical to understand what factors contribute to the magnitude of scarping, and what effect this has on dune systems to better manage coastal erosion into the future. Scarping occurs when foredunes are partially eroded by waves, generally during periods of high water level. The controls on the degree and magnitude of scarping examined include water level, foredune vegetation cover and spec
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Cohn, Nicholas, Bas Hoonhout, Evan Goldstein, et al. "Exploring Marine and Aeolian Controls on Coastal Foredune Growth Using a Coupled Numerical Model." Journal of Marine Science and Engineering 7, no. 1 (2019): 13. http://dx.doi.org/10.3390/jmse7010013.

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Coastal landscape change represents aggregated sediment transport gradients from spatially and temporally variable marine and aeolian forces. Numerous tools exist that independently simulate subaqueous and subaerial coastal profile change in response to these physical forces on a range of time scales. In this capacity, coastal foredunes have been treated primarily as wind-driven features. However, there are several marine controls on coastal foredune growth, such as sediment supply and moisture effects on aeolian processes. To improve understanding of interactions across the land-sea interface
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Kilibarda, Zoran, and Vesna Kilibarda. "Foredune and Beach Dynamics on the Southern Shores of Lake Michigan during Recent High Water Levels." Geosciences 12, no. 4 (2022): 151. http://dx.doi.org/10.3390/geosciences12040151.

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From 18 January 2013 (175.16 m a.s.l.) to 8 September 2020 (177.82 m a.s.l.), Lake Michigan experienced its fastest and highest rise (2.67 m) since 1860, when instrumental measurements began. Extensive foredunes developed since the last high lake levels began eroding in 1997 at fast rates. This study focuses on coastal morphodynamics along the 800 m coast within the central Indiana Dunes State Park on Lake Michigan’s southern shores during this time. Severe foredune erosion, in terms of total horizontal dune loss and total volume of eroded sand, occurred unevenly over the three-year period, bo
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Mickey, Rangley C., and Davina L. Passeri. "A Database of Topo-Bathy Cross-Shore Profiles and Characteristics for U.S. Atlantic and Gulf of Mexico Sandy Coastlines." Data 7, no. 7 (2022): 92. http://dx.doi.org/10.3390/data7070092.

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A database of seamless topographic and bathymetric cross-shore profiles along with metrics of the associated morphological characteristics based on the latest available lidar data ranging from 2011–2020 and bathymetry from the Continuously Updated Digital Elevation Model was developed for U.S. Atlantic and Gulf of Mexico open-ocean sandy coastlines. Cross-shore resolution ranges from 2.5 m for topographic and nearshore portions to 10 m for offshore portions. Topographic morphological characteristics include: foredune crest elevation, foredune toe elevation, foredune width, foredune volume, for
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Valdesolo, Tommaso, Silvia Del Vecchio, and Gabriella Buffa. "Patterns of Seed Dispersal in Coastal Dune Plant Communities." Sustainability 14, no. 17 (2022): 10983. http://dx.doi.org/10.3390/su141710983.

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Seed dispersal is a key determinant of species distribution, although it is still unclear how it contributes to species assembly in plant communities. We linked patterns of seed dispersal to coexisting species to investigate the role of dispersal in the species assembly process. We focused on 19 species coexisting in a foredune plant community, classified as “foredune foundation species”, “semi-fixed dune species,” and “alien species”. The number of seeds dispersed by the 19 species was monitored monthly in 25 plots for 12 months. Then we compared both dispersal strategies and dispersal phenol
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Dissertations / Theses on the topic "Coastal foredune"

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Knevel, Irma Cornelia. "The life history of selected coastal foredune species of South Africa." Thesis, Rhodes University, 2002. http://hdl.handle.net/10962/d1003776.

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South African dune fields are severely threatened by human expansion and in the long run the stabilisation of many dunes will be necessary. The alien grass Ammophila arenaria is the most important drift sand stabiliser at present in South Africa. Although not invasive, the current impact of A. arenaria on the dune systems of South Africa is considerable, and thus the stabilising benefit of the grass seemed to may be outweighed by its negative consequences. It is therefore preferable to use indigenous sand stabilising species. In order to define guidelines for the application of indigenous plan
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Rains, Bradley Jacob. "Effect of Barrier Height on Magnitude and Character of Hurricane Harvey Washover Fans, Matagorda Peninsula, TX." Thesis, University of North Texas, 2020. https://digital.library.unt.edu/ark:/67531/metadc1707228/.

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This study uses topographic profiles, washover fan volumes, and shoreline retreat rates to explore relationships between barrier types and Hurricane Harvey storm washover sedimentation. Pre- and post-Hurricane Harvey topographic profiles were created on 15 transects using Bare Earth LiDAR (2016) and surveyed elevations (2019). Depth and area of washover fan measurements were collected to estimate washover fan volumes. An inverse relationship was found between washover fan volume and pre- and post-storm barrier heights. Based on the topographic profiles, one section of shoreline had a scarp up
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LATELLA, MELISSA. "Integrated approaches for monitoring and modeling vegetation in riparian and coastal environments." Doctoral thesis, Politecnico di Torino, 2022. http://hdl.handle.net/11583/2971989.

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Bitencourt, Volney Junior Borges. "Geomorfologia e arquitetura deposicional de uma planície de cordões litorâneos lacustre, litoral norte do RS - Brasil." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2015. http://hdl.handle.net/10183/114396.

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Cordões litorâneos regressivos arenosos do tipo praia (beach ridge) e do tipo duna frontal (foredune ridge) são feições morfológicas comuns em costas deposicionais com abundância de sedimento. No presente estudo, a morfologia superficial, estratigrafia e a origem de uma planície de cordões ocorrentes na Lagoa dos Quadros, litoral norte do Rio Grande do Sul, são investigadas. Abordagens em superfície através de análises de fotografia aéreas, análises de imagens de satélite e altimetria de detalhe, em junção com dados em subsuperfície oriundos de perfilagens geofísica com uso de GPR e dados sedi
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Montreuil, Anne-Lise. "Aeolian dune development and evolution on a macro-tidal coast with a complex wind regime, Lincolnshire coast, UK." Thesis, Loughborough University, 2012. https://dspace.lboro.ac.uk/2134/10609.

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Coastal foredunes are natural aeolian bedforms located landward of the backshore and which interact continuously with the beach. Traditionally, coastal dunes have been associated with onshore winds, however they can be found under more complex wind regimes where offshore winds are common such as the UK East coast, Northern Ireland and New Zealand. This research investigates the ways in which foredune-beach interactions occur under a complex wind regime at a range of overlapping temporal and spatial scales and is innovative in that it explicitly links small-scale processes and morphodynamic beh
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Caruso, Laura <1977&gt. "Coastal foredunes as a resilient factor. The case of the Bevano river mouth natural reserve, Ravenna (Italy)." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2007. http://amsdottorato.unibo.it/1197/1/Laura_Caruso_Tesi_Dottorato.pdf.

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Caruso, Laura <1977&gt. "Coastal foredunes as a resilient factor. The case of the Bevano river mouth natural reserve, Ravenna (Italy)." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2007. http://amsdottorato.unibo.it/1197/.

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Knevel, Irma Cornelia. "The life history of selected coastal foredune species of South Africa /." 2001. http://eprints.ru.ac.za/29/.

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Rader, Alana Marie. "Foredune morphodynamics and seasonal sediment budget patterns: Humboldt Bay National Wildlife Refuge, Northern California, USA." Thesis, 2017. https://dspace.library.uvic.ca//handle/1828/8510.

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Delivery of sediment to beach-dune complexes along the northern California coast, as elsewhere, is controlled by littoral and aeolian processes governed largely by oceanic and meteorological conditions such as wind speed and direction, wave characteristics and water level fluctuations. Furthermore, patterns of sediment deposition on foredunes are controlled by the zonation, density and physical structure of dominant vegetation assemblages. This study explores the link between varying oceanic, meteorological and ecological patterns and coastal foredune morphodynamics at a site within the Humbol
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Ryu, Wansang. "A Typology of Foredune Textures: Sand Patches and Climate Controls." Thesis, 2012. http://hdl.handle.net/1969.1/148313.

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Foredunes are formed and developed in association with vegetation. A bare sand area has been viewed as a measure of dune mobility or activity and researched in association with climate controls: particularly wind power, annual mean precipitation, and temperature, expressed in annual mean potential evapotranspiration. There has been no research that utilized the patterns of bare sand areas to classify foredune areas in coastal dune systems and investigated climate controls related to sand patch patterns, or “foredune textures” such as size, number, and distribution of sand patches Four foredun
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Book chapters on the topic "Coastal foredune"

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Nordstrom, Karl F., and Nancy L. Jackson. "Foredune Restoration in Urban Settings." In Restoration of Coastal Dunes. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-33445-0_2.

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Feagin, Rusty. "Foredune Restoration Before and After Hurricanes: Inevitable Destruction, Certain Reconstruction." In Restoration of Coastal Dunes. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-33445-0_6.

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Lawlor, Paul, and Derek W. T. Jackson. "A Nature-Based Solution for Coastal Foredune Restoration: The Case Study of Maghery, County Donegal, Ireland." In Human-Nature Interactions. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-01980-7_32.

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Significance StatementClimate change has many negative impacts on coastal areas with sea level rise and more frequent and intense storms leading to higher rates of coastal flooding and erosion. Natural coastal features such as beaches and sand dune systems can boost resilience to climate change and provide an effective buffer against negative impacts. This case study from Maghery in Ireland demonstrates how a partnership of stakeholders comprising Local Government, Ulster University and the coastal community implemented a Nature-based Solution to regenerate a coastal foredune system in a Speci
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Psuty, N. P. "The Coastal Foredune: A Morphological Basis for Regional Coastal Dune Development." In Ecological Studies. Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-74002-5_2.

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Garcia-Lozano, Carla, Warren Meredith, Maria Marta Tonda, et al. "Evaluating the impact of sand fences on foredune recovery in Sant Pere Pescador beach (Costa Brava, Spain)." In Monitoring of Mediterranean Coastal Areas: Problems and Measurement Techniques. Firenze University Press, 2024. https://doi.org/10.36253/979-12-215-0556-6.63.

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Coastal dune systems have been significantly altered due to erosion from environmental and human factors, and nature-based solutions have become important in restoring these ecosystems in the face of climate change. The el Cortal de la Devesa beach (Gulf of Roses, NE Spain) has been the focus of such nature-based solutions with the installation of sand fences. Two campsites along this beach have implemented contrasting integration strategies over time. The Northern campsite has defined its boundaries and regulated beach access, while the Southern campsite did not. This study aimed to develop h
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Zhang, Wenyan, Ralf Schneider, Jan Harff, Birgit Hünicke, and Peter Fröhle. "Modelling of Medium-Term (Decadal) Coastal Foredune Morphodynamics- Historical Hindcast and Future Scenarios of the Świna Gate Barrier Coast (Southern Baltic Sea)." In Coastline Changes of the Baltic Sea from South to East. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-49894-2_7.

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Rozema, J., P. Bijwaard, G. Prast, and R. Broekman. "Ecophysiological adaptations of coastal halophytes from foredunes and salt marshes." In Ecology of coastal vegetation. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5524-0_54.

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Hesp, Patrick A., and Michael J. Hilton. "Restoration of Foredunes and Transgressive Dunefields: Case Studies from New Zealand." In Restoration of Coastal Dunes. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-33445-0_5.

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Preoteasa, Luminiţa, and Alfred Vespremeanu-Stroe. "Foredunes Dynamics on the Danube Delta Coast." In Springer Geography. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-32589-7_25.

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Psuty, Norbert P., and Tanya M. Silveira. "Restoration of Coastal Foredunes, a Geomorphological Perspective: Examples from New York and from New Jersey, USA." In Restoration of Coastal Dunes. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-33445-0_3.

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Conference papers on the topic "Coastal foredune"

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RUGGIERO, PETER, JEREMY MULL, PHOEBE ZARNETSKE, SALLY HACKER, and ERIC SEABLOOM. "INTERANNUAL TO DECADAL FOREDUNE EVOLUTION." In The Proceedings of the Coastal Sediments 2011. World Scientific Publishing Company, 2011. http://dx.doi.org/10.1142/9789814355537_0053.

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DOYLE, THOMAS B., and COLIN D. WOODROFFE. "WHAT ROLE DOES COASTAL VEGETATION PLAY IN FOREDUNE MORPHODYNAMICS?" In Coastal Sediments 2015. WORLD SCIENTIFIC, 2015. http://dx.doi.org/10.1142/9789814689977_0091.

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DAVIS, ELIZABETH H., NICHOLAS COHN, SELWYN S. HEMINWAY, JANELLE SKADEN, and CHRISTOPHER J. HEIN. "LINKING INTERNAL COASTAL FOREDUNE MOISTURE DYNAMICS TO EROSION VULNERABILITY." In Coastal Sediments 2023. WORLD SCIENTIFIC, 2023. http://dx.doi.org/10.1142/9789811275135_0062.

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LERMA, ALEXANDRE NICOLAE, BRUNO CASTELLE, DAVID ROSEBERY, et al. "FOREDUNE GUIDED REMOBILIZATION EXPERIMENTS ALONG THE SOUTHWEST COAST OF FRANCE." In Coastal Sediments 2023. WORLD SCIENTIFIC, 2023. http://dx.doi.org/10.1142/9789811275135_0060.

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BRODIE, KATHERINE L., and NICHOLAS J. SPORE. "FOREDUNE CLASSIFICATION AND STORM RESPONSE: AUTOMATED ANALYSIS OF TERRESTRIAL LIDAR DEMS." In Coastal Sediments 2015. WORLD SCIENTIFIC, 2015. http://dx.doi.org/10.1142/9789814689977_0041.

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Keijsers, J. G. S., A. Poortinga, M. J. P. M. Riksen, and A. V. de Groot. "Connecting aeolian sediment transport with foredune development." In NCK-days 2012 : Crossing borders in coastal research. University of Twente, Department of Water Engineering & Management, 2012. http://dx.doi.org/10.3990/2.187.

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Burnashov, Evgenii, Evgenii Burnashov, Konstantin Karmanov, and Konstantin Karmanov. "COMPARATIVE ANALYSIS OF THE INFLUENCE OF NATURAL AND ANTHROPOGENIC FACTORS ON THE VISTULA SPIT FOREDUNE EROSION (THE BALTIC SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b93da333dd5.38561507.

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The study gives quantitative estimation of natural landforms sensitivity of accumulative type coasts exposed to human influence. Foredune is an essential element of a morphological structure of thebarrier spits located at the Baltic Sea sand coasts. The study compares contribution of the beach erosion and deflation (soil drifting) to the foredune degradation on the sea shore of the barrier spit with or without the recreational impact. The analysis is performed for three typical polygons located on the Russian part of the Vistula Spit. Chosen polygons present shore segments with various intensi
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Burnashov, Evgenii, Evgenii Burnashov, Konstantin Karmanov, and Konstantin Karmanov. "COMPARATIVE ANALYSIS OF THE INFLUENCE OF NATURAL AND ANTHROPOGENIC FACTORS ON THE VISTULA SPIT FOREDUNE EROSION (THE BALTIC SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b4315ce62ab.

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The study gives quantitative estimation of natural landforms sensitivity of accumulative type coasts exposed to human influence. Foredune is an essential element of a morphological structure of thebarrier spits located at the Baltic Sea sand coasts. The study compares contribution of the beach erosion and deflation (soil drifting) to the foredune degradation on the sea shore of the barrier spit with or without the recreational impact. The analysis is performed for three typical polygons located on the Russian part of the Vistula Spit. Chosen polygons present shore segments with various intensi
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Davydov, Oleksiy, Alexander Stoyan, Alexander Murkalov, and Vasyli Chaus. "RESULTS OF AN EXPERIMENT ON THE CREATION OF AN ARTIFICIAL AEOLIAN FORM ALONG THE SEA COAST OF THE KINBURNSKA-POKROVSKA-DOVHIY COASTAL BARRIER, BLACK SEA." In 22nd SGEM International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022v/6.2/s26.58.

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Global climate changes, sea level rising, storm activity intensification, and increasing anthropogenic pressure are causing the activation of destructive processes along the coasts of the World Ocean. The corresponding processes are appeared at the most dangerous rates within the coastal barriers. Within the Black Sea, the total length of coastal barriers is 990 km, 703 km of which are within Ukraine. Corresponding barriers develop in conditions of active wave action and a general deficit of sediments. The maximum height of the relevany formations does not exceed 2.0 � 2.5 m, and the width is
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HEMINWAY, SELWYN S., ELIZABETH H. DAVIS, NICHOLAS COHN, JANELLE SKADEN, DYLAN ANDERSON, and CHRISTOPHER J. HEIN. "MODELED CHANGES IN FOREDUNE MORPHOLOGY INFLUENCED BY VARIABLE STORM INTENSITY AND SEA-LEVEL RISE." In Coastal Sediments 2023. WORLD SCIENTIFIC, 2023. http://dx.doi.org/10.1142/9789811275135_0064.

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Reports on the topic "Coastal foredune"

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Brodie, Katherine, Ian Conery, Nicholas Cohn, Nicholas Spore, and Margaret Palmsten. Spatial variability of coastal foredune evolution, part A : timescales of months to years. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/41322.

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Coastal foredunes are topographically high features that can reduce vulnerability to storm-related flooding hazards. While the dominant aeolian, hydrodynamic, and ecological processes leading to dune growth and erosion are fairly well-understood, predictive capabilities of spatial variations in dune evolution on management and engineering timescales (days to years) remain relatively poor. In this work, monthly high-resolution terrestrial lidar scans were used to quantify topographic and vegetation changes over a 2.5 year period along a micro-tidal intermediate beach and dune. Three-dimensional
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Palmsten, Margaret, Katherine Brodie, and Nicholas Spore. Coastal foredune evolution, Part 2 : modeling approaches for meso-scale morphologic evolution. Coastal and Hydraulics Laboratory (U.S.), 2017. http://dx.doi.org/10.21079/11681/21627.

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Brodie, Katherine, Margaret Palmsten, and Nicholas Spore. Coastal foredune evolution, Part 1 : environmental factors and forcing processes affecting morphological evolution. Coastal and Hydraulics Laboratory (U.S.), 2017. http://dx.doi.org/10.21079/11681/21468.

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Conlin, Matthew, Nicholas Cohn, and Peter Adams. Total water level controls on the trajectory of dune toe retreat. Engineer Research and Development Center (U.S.), 2023. http://dx.doi.org/10.21079/11681/47921.

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This study examines the trajectory (slope) of coastal foredune toe retreat in response to nine storm events that impacted the Outer Banks, North Carolina, USA. High resolution, three-dimensional, repeat mobile terrestrial lidar observations over a four kilometer stretch of coast were used to assess spatiotemporal beach and dune evolution at the storm timescale. Consistent with existing field observations from other sandy coastlines, an upward toe retreat was observed for most instances of dune retreat in the Outer Banks. However, these new topographic data indicate that the retreat can proceed
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Bryant, Duncan, Mary Bryant, and Alison Grzegorzewski. Erosion of coastal foredunes : a review on the effect of dune vegetation. Coastal and Hydraulics Laboratory (U.S.), 2017. http://dx.doi.org/10.21079/11681/21464.

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Renaud, Alexander, Michael Forte, Nicholas Spore, et al. Evaluation of Unmanned Aircraft Systems for flood risk management : results of terrain and structure assessments. Engineer Research and Development Center (U.S.), 2022. http://dx.doi.org/10.21079/11681/45000.

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The 2017 Duck Unmanned Aircraft Systems (UAS) Pilot Experiment was conducted by the US Army Engineer Research and Development Center (ERDC), Coastal and Hydraulics Laboratory, Field Research Facility (FRF), to assess the potential for different UAS to support US Army Corps of Engineers coastal and flood risk management. By involving participants from multiple ERDC laboratories, federal agencies, academia, and private industry, the work unit leads were able to leverage assets, resources, and expertise to assess data from multiple UAS. This report compares datasets from several UAS to assess the
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7

Boyle, Maxwell. Terrestrial vegetation monitoring at Cape Lookout National Seashore: 2022 data summary. National Park Service, 2024. http://dx.doi.org/10.36967/2303636.

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Parks within the Southeast Coast Network (SECN) host a diverse assemblage of plants and terrestrial vegetation communities. Vegetation communities are dynamic entities whose species composition, abundance, distribution, and structure are influenced by environmental factors and impacted over time by natural and anthropogenic disturbances. Determining trends in vegetation communities over time and identifying plant stressors is vital to understanding the ecological health of terrestrial ecosystems within SECN parks. Like most barrier islands along the southeastern coast, the vegetation communiti
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8

Inventory of lichen and bryophyte communities in the Yeon Unit of Lewis and Clark National Historical Park: Final report. National Park Service, 2023. http://dx.doi.org/10.36967/2301457.

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The 106-acre Yeon Unit of Lewis and Clark National Historic Park lies along the immediate coast eight miles north of Seaside, Oregon. The primary objective of these surveys was to capture the complete lichen and bryophyte flora of the Yeon property with focus on the remnant prairies and the salix swamp, report on any rare species observed or collected, and document the extent and population size of the rare lichen, Pannaria rubiginosa. Surveys were conducted in December 2021 and January 2022. While this report sufficiently characterizes the lichen and bryophyte flora of the Yeon property, it i
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