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1

Nardin, William, Sara Lera, and Jaap Nienhuis. "Effect of offshore waves and vegetation on the sediment budget in the Virginia Coast Reserve (VA)." Earth Surface Processes and Landforms 45, no. 12 (July 28, 2020): 3055–68. http://dx.doi.org/10.1002/esp.4951.

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2

Hayden, B. P., R. D. Dueser, J. T. Callahan, and H. H. Shugart. "Long-Term Research at the Virginia Coast Reserve." BioScience 41, no. 5 (May 1991): 310–18. http://dx.doi.org/10.2307/1311584.

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3

Hayden, Bruce P., Marcio C. F. V. Santos, Guofan Shao, and R. Craig Kochel. "Geomorphological controls on coastal vegetation at the Virginia Coast Reserve." Geomorphology 13, no. 1-4 (September 1995): 283–300. http://dx.doi.org/10.1016/0169-555x(95)00032-z.

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4

Mied, Richard P., William J. Schulz, Robert A. Handler, Charlotte M. Snow, Robert A. Fusina, and John H. Porter. "Remote and local forcing of a coastal lagoon: The Virginia Coast Reserve." Continental Shelf Research 30, no. 20 (December 2010): 2057–66. http://dx.doi.org/10.1016/j.csr.2010.10.005.

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5

Orth, RJ, and KJ McGlathery. "INTRODUCTION Eelgrass recovery in the coastal bays of the Virginia Coast Reserve, USA." Marine Ecology Progress Series 448 (February 23, 2012): 173–76. http://dx.doi.org/10.3354/meps09596.

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6

Johnson, Stephen R. "The Occurence of State Rare Species on Hog Island in the Virginia Coast Reserve." Bulletin of the Torrey Botanical Club 118, no. 3 (July 1991): 326. http://dx.doi.org/10.2307/2996647.

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7

Nardin, William, Laurel Larsen, Sergio Fagherazzi, and Patricia Wiberg. "Tradeoffs among hydrodynamics, sediment fluxes and vegetation community in the Virginia Coast Reserve, USA." Estuarine, Coastal and Shelf Science 210 (October 2018): 98–108. http://dx.doi.org/10.1016/j.ecss.2018.06.009.

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8

Knoff, A. J., S. A. Macko, and R. M. Erwin. "Diets of Nesting Laughing Gulls (Larus atricilla) at the Virginia Coast Reserve: Observations from Stable Isotope Analysis." Isotopes in Environmental and Health Studies 37, no. 1 (April 2001): 67–88. http://dx.doi.org/10.1080/10256010108033282.

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9

Bachmann, Charles M., C. Reid Nichols, Marcos J. Montes, Rong-Rong Li, Patrick Woodward, Robert A. Fusina, Wei Chen, et al. "Retrieval of Substrate Bearing Strength from Hyperspectral Imagery during the Virginia Coast Reserve (VCR’07) Multi-Sensor Campaign." Marine Geodesy 33, no. 2-3 (July 5, 2010): 101–16. http://dx.doi.org/10.1080/01490419.2010.492278.

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10

Goldstein, Evan B., Elsemarie V. Mullins, Laura J. Moore, Reuben G. Biel, Joseph K. Brown, Sally D. Hacker, Katya R. Jay, Rebecca S. Mostow, Peter Ruggiero, and Julie C. Zinnert. "Literature-based latitudinal distribution and possible range shifts of two US east coast dune grass species (Uniola paniculataandAmmophila breviligulata)." PeerJ 6 (June 8, 2018): e4932. http://dx.doi.org/10.7717/peerj.4932.

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Previous work on the US Atlantic coast has generally shown that coastal foredunes are dominated by two dune grass species,Ammophila breviligulata(American beachgrass) andUniola paniculata(sea oats). From Virginia northward,A. breviligulatadominates, whileU. paniculatais the dominant grass south of Virginia. Previous work suggests that these grasses influence the shape of coastal foredunes in species-specific ways, and that they respond differently to environmental stressors; thus, it is important to know which species dominates a given dune system. The range boundaries of these two species remains unclear given the lack of comprehensive surveys. In an attempt to determine these boundaries, we conducted a literature survey of 98 studies that either stated the range limits and/or included field-based studies/observations of the two grass species. We then produced an interactive map that summarizes the locations of the surveyed papers and books. The literature review suggests that the current southern range limit forA. breviligulatais Cape Fear, NC, and the northern range limit forU. paniculatais Assateague Island, on the Maryland and Virginia border. Our data suggest a northward expansion ofU. paniculata,possibly associated with warming trends observed near the northern range limit in Painter, VA. In contrast, the data regarding a range shift forA. breviligulataremain inconclusive. We also compare our literature-based map with geolocated records from the Global Biodiversity Information Facility and iNaturalist research grade crowd-sourced observations. We intend for our literature-based map to aid coastal researchers who are interested in the dynamics of these two species and the potential for their ranges to shift as a result of climate change.
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11

Woods, D. M., M. J. Pitcairn, D. G. Luster, and W. L. Bruckart. "First Report of Musk Thistle Rust (Puccinia carduorum) in California and Nevada." Plant Disease 86, no. 7 (July 2002): 814. http://dx.doi.org/10.1094/pdis.2002.86.7.814b.

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Musk thistle, Carduus nutans L., is an introduced weed of pastures, rangelands, and natural areas in much of North America. Puccinia carduorum Jacky, an autoecious rust fungus from Turkey, has been evaluated for biological control of musk thistle since 1978, including a field study near Blacksburg, VA, from 1987 to 1990. After release of the fungus in Virginia, rusted musk thistle was found in eight eastern states by 1992, in Missouri by 1994 (1), and in Oklahoma by 1997 (2). A rust disease was discovered on musk thistle near Mt. Shasta, CA, on 22 September 1998, and near Mogul, NV, on 12 August 1999. The pathogen was identified as P. carduorum on the basis of pathogenicity on musk thistle and urediniospore morphology (ovate spores, 21 μm diameter, three germ pores equatorial in location, and echinulations over the upper two-thirds to three-quarters of urediniospores). Ribosomal RNA internal transcribed spacer DNA sequences (ITS1 and ITS2) were identical to those from the isolate obtained after the field release in Virginia, verifying that the California isolate is P. carduorum. The initial California infestation was observed on a few plants late in the season, and by September 2000, nearly 100% of plants were infected. The occurrence of P. carduorum in California is apparently the result of natural, unaided spread of the fungus on musk thistle from the East Coast of the United States. References: (1) A. B. A. M. Baudoin and W. L. Bruckart. Plant Dis. 80:1193, 1996. (2) L. J. Littlefield et al. Plant Dis. 82:832, 1998.
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12

Bachmann, Charles M., Marcos J. Montes, Robert A. Fusina, Christopher Parrish, Jon Sellars, Alan Weidemann, Wesley Goode, et al. "Bathymetry Retrieval from Hyperspectral Imagery in the Very Shallow Water Limit: A Case Study from the 2007 Virginia Coast Reserve (VCR'07) Multi-Sensor Campaign." Marine Geodesy 33, no. 1 (February 26, 2010): 53–75. http://dx.doi.org/10.1080/01490410903534333.

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13

Eon, Rehman S., Charles M. Bachmann, Christopher S. Lapszynski, Anna Christina Tyler, and Sarah Goldsmith. "Retrieval of Sediment Filling Factor in a Salt Panne from Multi-View Hyperspectral Imagery." Remote Sensing 12, no. 3 (January 28, 2020): 422. http://dx.doi.org/10.3390/rs12030422.

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This work describes a study using multi-view hyperspectral imagery to retrieve sediment filling factor through inversion of a modified version of the Hapke radiative transfer model. We collected multi-view hyperspectral imagery from a hyperspectral imaging system mounted atop a telescopic mast from multiple locations and viewing angles of a salt panne on a barrier island at the Virginia Coast Reserve Long-Term Ecological Research site. We also collected ground truth data, including sediment bulk density and moisture content, within the common field of view of the collected hyperspectral imagery. For samples below a density threshold for coherent effects, originally predicted by Hapke, the retrieved sediment filling factor correlates well with directly measured sediment bulk density ( R 2 = 0.85 ). The majority of collected samples satisfied this condition. The onset of the threshold occurs at significantly higher filling factors than Hapke’s predictions for dry sediments because the salt panne sediment has significant moisture content. We applied our validated inversion model to successfully map sediment filling factor across the common region of overlap of the multi-view hyperspectral imagery of the salt panne.
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14

Jenkins, Willis. "Coastal Futures Conservatory." Environmental Humanities 13, no. 1 (May 1, 2021): 201–23. http://dx.doi.org/10.1215/22011919-8867274.

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Abstract This article develops an account of listening as a model for integrating inquiries into rapid environmental change from arts, sciences, and humanities. The account is structured around interpretation of the Coastal Futures Conservatory (CFC), an initiative for integrating arts and humanities into the Long-Term Ecological Research Project at the Virginia Coast Reserve. The CFC organizes collaborative inquiry and public engagement around several kinds of listening, from field recordings and designed listening stations as practices of attentiveness to scientific data by sonifying data sets, across disciplines by commissioning convergent lines of research from humanities and sciences, and across political boundaries by creating cross-coastal exchanges. Working from reflection on CFC practices, the author evaluates the potential and the limits of a pivot from ocular to aural metaphors of creating environmental knowledge as well as the potential and limits of listening as a model for integrating that knowledge. The author then questions integration as metaphor for multidisciplinary collaboration by testing its openness to listening beyond human worlds. The article closes by arguing for the role of contemplative practices in developing “transformative listening” as a way to connect environmental sciences with processes of moral and political formation.
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15

Hens, Luc, Nguyen An Thinh, Tran Hong Hanh, Ngo Sy Cuong, Tran Dinh Lan, Nguyen Van Thanh, and Dang Thanh Le. "Sea-level rise and resilience in Vietnam and the Asia-Pacific: A synthesis." VIETNAM JOURNAL OF EARTH SCIENCES 40, no. 2 (January 19, 2018): 127–53. http://dx.doi.org/10.15625/0866-7187/40/2/11107.

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Climate change induced sea-level rise (SLR) is on its increase globally. Regionally the lowlands of China, Vietnam, Bangladesh, and islands of the Malaysian, Indonesian and Philippine archipelagos are among the world’s most threatened regions. Sea-level rise has major impacts on the ecosystems and society. It threatens coastal populations, economic activities, and fragile ecosystems as mangroves, coastal salt-marches and wetlands. This paper provides a summary of the current state of knowledge of sea level-rise and its effects on both human and natural ecosystems. The focus is on coastal urban areas and low lying deltas in South-East Asia and Vietnam, as one of the most threatened areas in the world. About 3 mm per year reflects the growing consensus on the average SLR worldwide. The trend speeds up during recent decades. The figures are subject to local, temporal and methodological variation. In Vietnam the average values of 3.3 mm per year during the 1993-2014 period are above the worldwide average. Although a basic conceptual understanding exists that the increasing global frequency of the strongest tropical cyclones is related with the increasing temperature and SLR, this relationship is insufficiently understood. Moreover the precise, complex environmental, economic, social, and health impacts are currently unclear. SLR, storms and changing precipitation patterns increase flood risks, in particular in urban areas. Part of the current scientific debate is on how urban agglomeration can be made more resilient to flood risks. Where originally mainly technical interventions dominated this discussion, it becomes increasingly clear that proactive special planning, flood defense, flood risk mitigation, flood preparation, and flood recovery are important, but costly instruments. Next to the main focus on SLR and its effects on resilience, the paper reviews main SLR associated impacts: Floods and inundation, salinization, shoreline change, and effects on mangroves and wetlands. The hazards of SLR related floods increase fastest in urban areas. This is related with both the increasing surface major cities are expected to occupy during the decades to come and the increasing coastal population. In particular Asia and its megacities in the southern part of the continent are increasingly at risk. The discussion points to complexity, inter-disciplinarity, and the related uncertainty, as core characteristics. An integrated combination of mitigation, adaptation and resilience measures is currently considered as the most indicated way to resist SLR today and in the near future.References Aerts J.C.J.H., Hassan A., Savenije H.H.G., Khan M.F., 2000. Using GIS tools and rapid assessment techniques for determining salt intrusion: Stream a river basin management instrument. 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