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Автор: Grafiati
Опубліковано: 27 липня 2024
Оновлено: 29 липня 2024

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Статті в журналах з теми "New hampshire, maps"

1

Mueller, Charles S., Oliver S. Boyd, Mark D. Petersen, Morgan P. Moschetti, Sanaz Rezaeian, and Allison M. Shumway. "Seismic Hazard in the Eastern United States." Earthquake Spectra 31, no. 1_suppl (December 2015): S85—S107. http://dx.doi.org/10.1193/110414eqs182m.

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The U.S. Geological Survey seismic hazard maps for the central and eastern United States were updated in 2014. We analyze results and changes for the eastern part of the region. Ratio maps are presented, along with tables of ground motions and deaggregations for selected cities. The Charleston fault model was revised, and a new fault source for Charlevoix was added. Background seismicity sources utilized an updated catalog, revised completeness and recurrence models, and a new adaptive smoothing procedure. Maximum-magnitude models and ground motion models were also updated. Broad, regional hazard reductions of 5%–20% are mostly attributed to new ground motion models with stronger near-source attenuation. The revised Charleston fault geometry redistributes local hazard, and the new Charlevoix source increases hazard in northern New England. Strong increases in mid- to high-frequency hazard at some locations—for example, southern New Hampshire, central Virginia, and eastern Tennessee—are attributed to updated catalogs and/or smoothing.
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2

Klymko, John, and S. A. Marshall. "Review of the Nearctic Lonchopteridae (Diptera), including descriptions of three new species." Canadian Entomologist 140, no. 6 (December 2008): 649–73. http://dx.doi.org/10.4039/n08-034.

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AbstractThe Nearctic species of Lonchoptera Meigen are reviewed, including three new species: L. barberi Klymko sp. nov. from Manitoba, Newfoundland, Ontario, Quebec, Iowa, Michigan, Minnesota, and New Hampshire, L. megaloba Klymko sp. nov. from British Columbia and California, and L. longiphallus Klymko sp. nov. from British Columbia and the Northwest Territories. Lonchoptera borealis Curran is proposed as a new junior synonym of L. impicta Zetterstedt, and L. occidentalis Curran is proposed as a new junior synonym of L. uniseta Curran. Lonchoptera nigrociliata Duda, formerly known only from the Palaearctic Region, is recorded from the Yukon and Alaska. Descriptions, a key, and Nearctic distribution maps are presented. Phylogenetic relationships are briefly discussed and two sister species pairs are documented.
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3

Andrew, Angeline S., Meifang Li, Xun Shi, Judy R. Rees, Karen M. Craver, and Jonathan M. Petali. "Kidney Cancer Risk Associated with Historic Groundwater Trichloroethylene Contamination." International Journal of Environmental Research and Public Health 19, no. 2 (January 6, 2022): 618. http://dx.doi.org/10.3390/ijerph19020618.

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Trichloroethylene (TCE) is a well-documented kidney carcinogen based on a substantial body of evidence including mechanistic and animal studies, as well as reports from occupational settings. However, the cancer risks for those in residential exposures such as TCE contamination in groundwater are much less clear. The objective of this study was to perform a detailed spatio-temporal analysis of estimated residential TCE exposure in New Hampshire, US. We identified kidney cancer cases (n = 292) and age-, gender-matched controls (n = 448) from the Dartmouth-Hitchcock Health System and queried a commercial financial database for address histories. We used publically available data on TCE levels in groundwater measured at contaminated sites in New Hampshire and then modeled the spatial dispersion and temporal decay. We overlaid geospatial residential locations of cases and controls with yearly maps of estimated TCE levels to estimate median exposures over the 5, 10, and 15-year epochs before diagnosis. The 50th–75th percentile of estimated residential exposure over a 15-year period was associated with increased kidney cancer risk (adjusted Odds Ratio (OR) 1.78 95% CI 1.05–3.03), compared to <50th percentile. This finding supports the need for groundwater monitoring of TCE contaminated sites to identify potential public health risks.
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4

Hall, Dorothy K., Andrew B. Tait, James L. Foster, Alfred T. C. Chang, and Milan Allen. "Intercomparison of satellite-derived snow-cover maps." Annals of Glaciology 31 (2000): 369–76. http://dx.doi.org/10.3189/172756400781820066.

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AbstractIn anticipation of the launch of the Earth Observing System (EOS) Terra, and the Aqua spacecraft in 1999 and 2000, respectively, efforts are ongoing to determine errors of satellite-derived snow-cover maps. EOS Moderate Resolution Imaging Spectrora-diometer (MODIS) and Advanced Microwave Scanning Radiometer-E (AMSR-E) snow-cover products will be produced. For this study we compare snow maps covering the same study areas in Canada and the United States, acquired from different sensors using different snow-mapping algorithms. Four locations are studied: (1) Saskatchewan, Canada; (2) New England (New Hampshire, Vermont and Massachusetts) and eastern New York; (3) central Idaho and western Montana; and (4) North and South Dakota. Snow maps were produced using a prototype MODIS snow-mapping algorithm from Landsat Thematic Mapper (TM) scenes of each study area at 30 m and when the TM data were degraded to 1 km resolution. U.S. National Operational Hydrologic Remote Sensing Center (NOHRSC) 1km resolution snow maps were also used, as were snow maps derived from 0.5° × 0.5° resolution Special Sensor Microwave Imager (SSM/I) data. A land-cover map derived from the International Geosphere-Biosphere Program land-cover map of North America was also registered to the scenes. The TM, NOHRSC and SSM/ I snow maps, and land-cover maps were compared digitally. In most cases, TM-derived maps show less snow cover than the NOHRSC and SSM/I maps because areas of incomplete snow cover in forests (e.g. tree canopies, branches and trunks) are seen in the TM data but not in the coarser-resolution maps which may map the areas as completely snow-covered. The snow maps generally agree with respect to the spatial variability of the snow cover. The 30 m resolutionTM data provide the most accurate snow maps, and are thus used as the baseline for comparison with the other maps. Results show that the changes in amount of snow cover, as compared to to the 30 m resolution TM maps, are lowest using the TM 1km resolution maps, at 0–40%. The greatest change (>100%) is found in the New England study area, probably due to the presence of patchy snow cover. A scene with patchy snow cover is more difficult to map accurately than is a scene with a well-defined snowline such as is found on the North and South Dakota scene where the changes were 0–40%. There are also some important differences in the amount of snow mapped using the two different SSM/I algorithms because they utilize different channels.
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Anderson, Nathaniel M., René H. Germain, and Eddie Bevilacqua. "Geographic Information System-Based Spatial Analysis of Sawmill Wood Procurement." Journal of Forestry 109, no. 1 (January 1, 2011): 34–42. http://dx.doi.org/10.1093/jof/109.1.34.

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Abstract In the sawmill sector of the forest products industry, the clustering of mills and wide variation in forest stocking and ownership result in sawlog markets that are complex and spatially differentiated. Despite the inherent spatial attributes of markets for stumpage and logs, few studies have used geospatial methods to examine wood procurement in detail across political boundaries. This article provides a visual representation of wood procurement pressure across the Northern Forest region of the northeastern United States based on a spatial analysis of woodshed maps provided by 273 sawmills in the United States and Canada. The analysis also includes the predicted woodsheds of 280 nonrespondent mills, which were modeled based on mill characteristics and location. In general, maps emphasize the magnitude of softwood procurement on industrial and investment-oriented forestlands in northern Maine, but also highlight distinct spatial procurement patterns in New York, Vermont, and New Hampshire. Sensitivity analyses of woodshed boundary uncertainty suggest that procurement pressure in existing hotspots will intensify if procurement range is restricted by high transportation costs. The methods used to visualize resource procurement in this study have the potential to benefit a broad range of stakeholders including industry, policymakers, and landowners.
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Desmarais, Norman. "Historic USGS Maps of New England & New York2010198Historic USGS Maps of New England & New York. URL: http://docs.unh.edu/nhtopos/nhtopos.htm: University of New Hampshire Dimond Library, Documents Department & Data Center Last visited December 2009. Gratis." Reference Reviews 24, no. 4 (May 4, 2010): 56. http://dx.doi.org/10.1108/09504121011045944.

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7

Davis, P. Thompson. "Cirques of the Presidential Range, New Hampshire, and surrounding alpine areas in the northeastern United States." Géographie physique et Quaternaire 53, no. 1 (October 2, 2002): 25–45. http://dx.doi.org/10.7202/004784ar.

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Abstract Evidence for rejuvenation of cirque glaciers following wastage of continental ice remains elusive for the Presidential Range and Mount Moosilauke of New Hampshire, Mount Katahdin and the Longfellow Mountains of Maine, and the Adirondack Mountains of New York. At Ritterbush Pond in the northern Green Mountains of Vermont, radiocarbon ages from lake sediment cores suggest that a low-altitude valley head, located up- valley of a series of cross-valley moraines, was ice-free by 11,940 14 C yrs BP (Bierman et al. , 1997). Although some workers argue that these moraines in Vermont are evidence for cirque glaciation, the moraines could have been formed by a tongue of continental ice during deglaciation. At Johnson Hollow Brook valley in the Catskill Mountains of New York, a radiocarbon age from basal sediments in a pond dammed by a moraine suggests that glacier ice may have persisted until 10,860 14 C yrs BP (Lederer and Rodbell, 1998). Because this moraine appears to have been deposited by a cirque glacier, the radiocarbon age provides the best evidence in the northeastern United States for cirque glaciation post-dating recession of continental ice. Cirque morphometric data, compiled from newly available topographic maps, add to the conundrum that these two sites in the Green and Catskill Mountains should not be nearly as favorable for maintaining local glaciers post- dating icesheet recession as higher-altitude and better-developed cirques in the Presidential Range and Mount Katahdin, where evidence for post-icesheet cirque glaciers is lacking.
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8

Semple, John C., and Rachel E. Cook. "Cytogeography of Solidago sect. Erectae, sect. Villosicarpae, sect. Squarrosae, and sect. Brintonia (Asteraceae: Astereae)." Taxonomy 2, no. 3 (July 3, 2022): 261–78. http://dx.doi.org/10.3390/taxonomy2030021.

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Chromosome numbers are reported for 67 individuals of 13 species of Solidago sect. Erectae, S. sect. Squarrosae, and S. sect. Villosicarpae from 65 locations in eastern Canada and the eastern United States: S. bicolor, S. erecta, S. hispida, S. jejunifolia, S. pallida, S. puberula, S. pulverulenta, S. rigidiuscula, S. roanensis, S. sciaphila, S. speciosa, S. squarrosa, and S. villosicarpa. Cytogeography maps based on new reports and all 258 previously published reports from 230 locations for the three sections plus S. sect. Brintonia (S. discoidea) are presented for 20 of the 30 species in the four closely related sections. The following are either first documented reports for the taxon or just first counts for a taxon from particular provinces and states: Solidago bicolor, 2n = 18 from Nova Scotia and Prince Edward Island; S. hispida var. hispida, 2n = 18 from New Hampshire, New Brunswick, and Wisconsin; S. jejunifolia, 2n = 18 from Michigan and Minnesota; S. pallida, 2n = 18 from Wyoming; S. puberula, 2n = 18 from Pennsylvania, Prince Edward Island, and Virginia; and first reports for S. sciaphila, 2n = 36 from Iowa, Illinois, and Wisconsin.
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9

Hundley, Steve, Karen Dudley, and Laura Morton. "Accuracy of Soil Line Placement on Site-Specific Soil Maps Based on the Site-Specific Soil Mapping Standards for New Hampshire and Vermont." Soil Horizons 41, no. 2 (2000): 21. http://dx.doi.org/10.2136/sh2000.2.0021.

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10

Klimaszewski, Jan, Greg Pohl, and Georges Pelletier. "Revision of the Nearctic Silusa (Coleoptera, Staphylinidae, Aleocharinae)." Canadian Entomologist 135, no. 2 (April 2003): 159–86. http://dx.doi.org/10.4039/n02-027.

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AbstractA revision of the Canadian species of the genus Silusa Erichson is presented. In this contribution, we treat six species recently discovered in Canada, one of which is a new species from Alberta, Silusa langori Klimaszewski sp. nov. The distribution records for two species are greatly expanded. Silusa californica Bernhauer is now known from Alaska, Minnesota, Alberta, Quebec, New Brunswick, and Nova Scotia (previous records: British Columbia, California). Silusa vesperis Casey is now known from Washington and British Columbia (previous record: California). For two other species, there are first records for Canada and one new United States state record. Silusa alternans Sachse is now known from Quebec, New Brunswick, Nova Scotia, and New Hampshire (previous records: Georgia, New York), and Silusa densa Fenyes is now known from Alberta (previous record: California). Silusa valens Casey is here considered as a synonym of S. alternans. Silusa rutilans Casey and S. modica Casey are confirmed to belong to Leptusa Kraatz, and both are here considered as new synonyms of Leptusa canonica Casey. Silusa gracilis Sachse and S. nanula Casey are also confirmed to belong to the genus Leptusa. The following lectotypes are newly designated for species described on the basis of syntypes: S. alternans Sachse and S. californica Bernhauer. New data are provided on the systematics, relationships, bionomics, and distribution for all Nearctic species of America north of Mexico. Diagnoses and illustrations of external and genital features are provided for all species, and the distribution of each is discussed and shown on maps. A key to the species occurring in Canada is presented.
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Дисертації з теми "New hampshire, maps"

1

Johnson, Alexander James Cook. "Charting the imperial will : colonial administration & the General Survey of British North America, 1764-1775." Thesis, University of Exeter, 2011. http://hdl.handle.net/10036/3458.

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This dissertation explores how colonial administrators on each side of the Atlantic used the British Survey of North America to serve their governments’ as well as their personal objectives. Specifically, it connects the execution and oversight of the General Survey in the northern and southern theatres, along with the intelligence it provided, with the actions of key decision-makers and influencers, including the Presidents of the Board of Trade (latterly, the Secretaries of the American Department) and key provincial governors. Having abandoned their posture of ‘Salutary Neglect’ towards colonial affairs in favour of one that proactively and more centrally sought ways to develop and exploit their North American assets following the Severn Years’ War, the British needed better geographic information to guide their decision making. Thus, the General Survey of British North America, under the umbrella of the Board of Trade, was conceived. Officially sponsored from 1764-1775, the programme aimed to survey and analyse the attributes and economic potential of Britain’s newly acquired regions in North America, leading to an accurate general map of their North American empire when joined to other regional mapping programmes. The onset of the American Revolution brought an inevitable end to the General Survey before a connected map could be completed. Under the excellent leadership of Samuel Holland, the surveyor general of the Northern District, however, the British administration received surveys and reports that were of great relevance to high-level administration. In the Southern District, Holland’s counterpart, the mercurial William Gerard De Brahm, while producing reports of high quality, was less able to juggle the often conflicting priorities of provincial and London-based stakeholders. Consequently, results were less successful. De Brahm was recalled in 1771, leaving others to complete the work.
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Книги з теми "New hampshire, maps"

1

Company, DeLorme Publishing. The New Hampshire atlas and gazetteer. 7th ed. Freeport, Me: The Company, 1986.

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2

Rosenberg, Gerald L. Soil survey of Cheshire County, New Hampshire. [Washington, D.C.?]: The Service, 1989.

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3

Kelsea, Russell J. Soil survey of Rockingham County, New Hampshire. [Washington, D.C.?]: The Service, 1994.

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4

Homer, Joseph W. Soil survey of Grafton County area, New Hampshire. [Washington, D.C.]: The Service, 1999.

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5

Handler, John F. Soil survey of Hillsborough County, New Hampshire, western part. [Washington, D.C.?]: The Service, 1985.

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6

Society of Soil Scientists of Northern New England. High intensity soil maps for New Hampshire: Standards and origins. [New Hampshire?]: The Society, 1987.

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7

Koteff, Carl. Surficial geologic map of the Kingston quadrangle, Rockingham County, New Hampshire. Reston, VA: U.S. Geological Survey, 1994.

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8

Koteff, Carl. Surficial geologic map of the Townsend quadrangle, Middlesex and Worcester counties, Massachusetts and Hillsborough County, New Hampshire. Reston, VA: U.S. Geological Survey, 1990.

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9

Pohn, Howard A. Radar and landsat lineament maps of the Glens Falls 1 x 2 quadrangle, New York, Vermont, and New Hampshire. [Denver, Colo.?]: Dept. of the Interior, U.S. Geological Survey, 1986.

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10

Pohn, Howard A. Radar and landsat lineament maps of the Glens Falls 1p0s x 2p0s quadrangle, New York, Vermont, and New Hampshire. [Denver, Colo.?]: Dept. of the Interior, U.S. Geological Survey, 1986.

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Частини книг з теми "New hampshire, maps"

1

Jamieson, Kathleen Hall. "Solutions or Strategy?" In Dirty Politics, 189–200. Oxford University PressNew York, NY, 1992. http://dx.doi.org/10.1093/oso/9780195078541.003.0009.

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Abstract Two moments in the 1980 campaign illustrate the differences between a focus on strategy and a focus on problems, candidates’ proposed solutions, and their relevant performance in the past. The first occurred on the morning of the New Hampshire primary. On the Democratic side, Senator Edward Kennedy (D. Mass.) was facing incumbent president Jimmy Carter. As New Hampshire voters were drinking their morning cup of coffee, Tom Brokaw was interviewing Kennedy on NBC. Were a therapist eavesdropping on the conversation, she might ask, Can this relationship be saved? After all, their goals are fundamentally incompatible. Brokaw wants to know what Kennedy will do if he loses to Carter in New Hampshire; Kennedy wants to persuade New Hampshire Democrats that his proposed policies are preferable to the Georgian’s.
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2

Brooks, Lisa. "The Northern Front: Beyond Replacement Narratives." In Our Beloved Kin. Yale University Press, 2018. http://dx.doi.org/10.12987/yale/9780300196733.003.0013.

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This book concludes where it opened, on the Northern Front of Wabanaki, where the war, and the negotiation of peace, continued long past the summer of 1676. This chapter focuses on a wave of raids that began on the Wabanaki coast, on the same day that Metacom was killed, as well as the efforts of multiple Penacook and Abenaki leaders to end the conflict through diplomacy. It highlights the complex context behind the “surprisal” at Cocheco, involving New Hampshire trader Richard Waldron, and explores the response of Indigenous leaders on the Kennebec River. The chapter concludes with the little-known treaties of Pemaquid and Casco Bay in 1677 and 1678, exploring a wide map of Indigenous communication, diplomacy, and alliance. This wider map also enables acknowledgment of the role of the colonies of New York and New France in both diplomacy and war.
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3

"Benthic Habitats and the Effects of Fishing." In Benthic Habitats and the Effects of Fishing, edited by George R. Cutter, Yuri Rzhanov, Larry A. Mayer, and Raymond E. Grizzle. American Fisheries Society, 2005. http://dx.doi.org/10.47886/9781888569605.ch16.

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<strong><em>Abstract. </em></strong>Subtidal benthic habitats from the Piscataqua River, New Hampshire and Maine, have been delineated by an automated segmentation technique using bathymetry derived from multibeam echo sounder data. The map, produced by segmentation of seafloor textures, represents a hypothetical benthic habitat map that requires ground-truthing. Video mosaics are being used to ground-truth substrate composition and transitions apparent in the bathymetry data map and to describe biological features and organism occurrences and densities. Here, we describe the utility of video mosaics for ground-truthing benthic habitat characteristics and present two examples of their use. Video mosaics acquired along two transects in the Piscataqua River were used to detect substrate transitions apparent in the bathymetry that were identified as distinct hypothetical habitat types and to quantitatively assess coverages of distinct sediment conditions, density of megafaunal organisms (lobsters), and bioturbational features (crab feeding pits).
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Smith, Ronald A. "Sport, the Extracurriculum, and the Idea of Freedom." In Sports And Freedom, 13–25. Oxford University PressNew York, NY, 1990. http://dx.doi.org/10.1093/oso/9780195065824.003.0002.

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Abstract Foot Ball Was Played every fair fall day at Dartmouth College in the mid-1830s. Ex-president S. C. Bartlett recalled his earlier fresh man playing days at the New Hampshire institution. He remem bered a senior who used “ stupendous boots he had made on purpose with soles fully a half inch thick. “ Bartlett, nearly six decades after the event, could still see the hulking upperclassman as he stood “ on the extreme edge of a dense, surging mass of struggles, the foot-ball far out of sight in the centre, but the boots going like a horizontal trip-hammer “ in one of those glorious class battles.1 It appeared at least as important to incapacitate the lowly “frosh “ as it was to score the next goal.
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Morgan, David. "The Commerce of Images and Adventist Piety." In Protestants & Pictures Religion, Visual Culture, and the Age of American Mass Production, 159–98. Oxford University PressNew York, NY, 1999. http://dx.doi.org/10.1093/oso/9780195130294.003.0006.

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Abstract From its inception during the Millerite period to its reinstitution among Adventists after the failure of the Second Coming of Christ to occur as Miller had predicted, the prophetic chart became a proudly displayed mark of difference. This is not surprising when we remember that Millerism developed an oppositional consciousness as it was attacked by Protestant orthodoxy. Charles Fitch, who had designed the most popular chart in 1842, undertook in the summer of 1843 his “Out of Babylon” crusade, which drove a wedge between the Protestant mainstream and the Adventist movement (much to Miller’s regret).1 By 1844 the chart served to distinguish insider from outsider, as the daughter of Millerite preacher Joseph Marsh recalled when she wrote in 1886, about the charts covering the walls of her childhood home, that “those realistic conceptions of the supernatural bewilder[ed] one uninitiated in their mysteries.”2 Adventist imagery and charts often appeared at the intersection of conflict. A major assault on Millerite doctrine by the Baptist pastorJohn Dowling, which was reprinted on the front page of a New York Tribune extra, included a reproduction of a chart, “Daniel’s Visions,” first published in the Midnight Cry (fig. 69).3 Opponents seized on the Millerite imagery as a means of public identification and ridicule of Millerite beliefs. One broadside lampooning Miller as the “high priest of Millerism” preaching at the East Kingston, New Hampshire, camp meeting in June and July of 1842 (where Fitch also presented the painted chart) included the tenhorned beast representing pagan Rome.
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Cumbler, John T. "Cities and Industry, Sewage and Waste." In Reasonable Use. Oxford University Press, 2001. http://dx.doi.org/10.1093/oso/9780195138139.003.0007.

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In 1886, James Olcott, a farmer, “having been bred in the old anti-slavery reform,” gave a speech before the Agricultural Board of Connecticut. Recalling an earlier age, he encouraged his audience and “the common people” of Connecticut to “agitate, agitate,” in order to “cleanse” the state of the “social evil” of the pollution “by sewage from families and factories, festering in every pool, and mill pond—formerly trout holes.” Olcott reminded the farmers that “our best hold on polluted streams reform lies in the fact that the mischief has brought on us its calamitous consequences in this country with such rapidity that men and women too not very greyhaired and in full bodily and mental vigor can shut their eyes and review the whole matter from its beginning.” The history Olcott conjured up was the transformation of a clean, clear environment from “one of the most salubrious to one of the worst in the world.” The change was intimately linked to the rise of industrial cities like Bellows Falls, Chicopee, Hartford, New Britain, and Holyoke. Although Olcott’s remembrance of the past was partly colored by romantic notions of a purer age, the pollution he pointed to was indeed a problem of growing obviousness and concern. Reflecting the rapid change that had occurred over the last quarter century, the Massachusetts State Board of Health complained that with the growth of densely populated industrial cities, the old habits of disposing of waste contributed to “a large part of the filth in our state,” and that “often the water which is used for domestic purposes [is disposed of] by being thrown upon the surface of the ground, or collected in loosewalled vaults and cesspools,” which might have been acceptable in a rural community but caused concern in the new industrial cities. As the New Hampshire Board of Health noted in 1887, looking back over the last few decades, “when men mass, . . . the conditions at once become aggravated. . . . Man comes in with his artificial constructions and sweeps away much of this economy of nature.”
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"Benthic Habitats and the Effects of Fishing." In Benthic Habitats and the Effects of Fishing, edited by Raymond E. Grizzle, Larry G. Ward, Jamie R. Adams, Semme J. Dijkstra, and Brian Smith. American Fisheries Society, 2005. http://dx.doi.org/10.47886/9781888569605.ch13.

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<strong><em>Abstract. </em></strong>Populations of the eastern oyster <em>Crassostrea virginica </em>have been in long-term decline in most areas. A major hindrance to effective oyster management has been lack of a methodology for accurately and economically obtaining data on their distribution and abundance patterns. Here, we describe early results from studies aimed at development of a mapping and monitoring protocol involving acoustic techniques, underwater videography, and destructive sampling (excavated quadrats). Two subtidal reefs in Great Bay, New Hampshire, were mapped with side-scan sonar and with videography by systematically imaging multiple sampling cells in a grid covering the same areas. A single deployment was made in each cell, and a 5–10-s recording was made of a 0.25-m<sup>2</sup> area; the location of each image was determined using a differential global position system. A still image was produced for each of the cells and all (<em>n </em>= 40 or 44) were combined into a single photomontage overlaid onto a geo-referenced base map for each reef using ArcView geographic information system. Quadrat (0.25 m<sup>2</sup>) samples were excavated from 9 or 10 of the imaged areas on each reef, and all live oysters were counted and measured. Intercomparisons of the acoustic, video, and quadrat data suggest: (1) acoustic techniques and systematic videography can readily delimit the boundaries of oyster reefs; (2) systematic videography can yield quantitative data on shell densities and information on reef structure; and (3) some combination of acoustics, systematic videography, and destructive sampling can provide spatially detailed information on oyster reef characteristics.
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Тези доповідей конференцій з теми "New hampshire, maps"

1

Nedyalkov, Ivaylo, and Martin Wosnik. "Adaptive-Time-Step High-Frame-Rate Particle Image Velocimetry." In ASME 2016 Fluids Engineering Division Summer Meeting collocated with the ASME 2016 Heat Transfer Summer Conference and the ASME 2016 14th International Conference on Nanochannels, Microchannels, and Minichannels. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/fedsm2016-7748.

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With the availability of high-frame-rate (HFR) PIV systems, it is possible to capture time series of particle images at rates which can exceed the necessary frequency to temporally resolve essential flow. In this case, some of the recorded frames can be skipped, in order to obtain an adequate time step between two images, leading to favorable values for pixel displacement. In this paper a technique for decreasing pixel locking in complex flows based on an adaptive time step processing procedure is proposed. If PIV data are taken at much higher frequency than needed, the processing can be repeated for multiple time steps, ensuring the optimal pixel displacement for every interrogation spot. A smaller time step is used for large velocities and larger time steps are used in the areas of low velocity. To illustrate this technique, a sample data set was acquired of the flow on the suction side and the region just downstream of a NACA 0015 hydrofoil at a high angle of attack (16 degrees), ensuring a wide range of velocities within the PIV field of view. The experiments were performed in the University of New Hampshire High-Speed Cavitation Tunnel – HiCaT, at a comparatively low speed (2 m/s) in order to increase the range of possible time steps for post processing. HFR PIV data were obtained at 1800 frames per second for a field of view of approximately 100 mm × 100 mm. The data were processed multiple times, each time skipping between 0 and 19 frames, resulting in time steps between 1 to 20 times of the original time step between two images. As expected, there is a significant difference between the results for mean velocities with different time step processing, most notably in the region of the suction side of the foil. The RMS velocity fields also show a similar trend. In order to obtain a more accurate representation of the mean flow, the data for each interrogation spot were combined based on the pixel displacement values. The resulting velocity field was compared to that obtained with single-time-step PIV. A “map” was created showing what time step was selected for each interrogation spot. Suggestions were made on what time steps should be selected for the post processing in order to decrease the post processing computational time. A discussion was provided on the feasibility of using the technique for instantaneous velocity fields. Using ATS PIV may be beneficial in flows where both large and small velocities are of importance, e.g., flows with separation.
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Nedyalkov, Ivaylo, Ian Gagnon, Jesse Shull, John Brindley, and Martin Wosnik. "Wingtip Devices for Tidal Turbines: Performance Improvement and Cavitation Mitigation." In ASME 2016 Fluids Engineering Division Summer Meeting collocated with the ASME 2016 Heat Transfer Summer Conference and the ASME 2016 14th International Conference on Nanochannels, Microchannels, and Minichannels. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/fedsm2016-7750.

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Wingtip devices are common in aeronautical applications and are increasingly used on wind turbines. However, their use in hydrokinetic energy conversion applications such as tidal turbines to date is minimal, due to the concern for increased bio-fouling and also the fact that there is little or no data publically available describing their cavitation characteristics. In this study, three wingtip designs were considered for hydrokinetic turbine applications: a plain foil with a rounded tip (considered the reference case), a generic wingtip device (a winglet), and a novel “split-tip” device. The tips were studied numerically and experimentally at different angles of attack. The numerical simulations were performed in OpenFOAM using the k-omega SST model to predict the lift and drag characteristics of a “base” foil with each of the three wingtip devices. Additionally the pressure and vorticity were observed. Experiments were conducted in the University of New Hampshire High-Speed Cavitation Tunnel – HiCaT. A modular experimental test bed with an elliptical foil section was developed specifically for the study. The test bed extends to the centerline of the tunnel where wingtips are attached, and has four small-diameter tube openings to accommodate pressure measurements and/or mass injection studies. Water tunnel data were obtained for lift, and cavitation inception, and compared to the numerical simulations. The numerical results show decreased vorticity with presence of the wingtip devices, however, the advantage of using wingtips for decreasing drag and increasing lift forces is not conclusively exhibited. The experimental measurements suggest that there is a significant suppression of tip vortex cavitation with the use of wingtip devices at high angles of attack (around 10 degrees), but the advantage of using the wingtip devices diminishes at lower angles of attack. It was shown by Arndt [1] that tip-vortex cavitation on hydrofoils can be related to the lift coefficient and the Reynolds number, where the cavitation index at inception is proportional to the square of the section lift coefficient and the Reynolds number based on hydrofoil chord, taken to the power m. The power exponent m has been generally accepted to be approximately 0.4. This relation is made into an equation via a coefficient of proportionality K, which depends on the wingtip and foil section geometry, and has been empirically determined to have values between 0.025 and 0.056 for previously investigated wings. While the value of the coefficient K for the reference wing tip remained comparatively constant for the range of conditions investigated (angles of attack, Reynolds numbers), it varied significantly for the foil terminated by the winglet. This may be due to the non-elliptical load distribution in the span-wise direction, but also raises the question whether the standard tip-vortex cavitation correlation for hydrofoils is applicable for general wingtip devices.
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Звіти організацій з теми "New hampshire, maps"

1

Bouguer gravity anomaly maps and four derivative maps of New Hampshire, Vermont, and vicinity. US Geological Survey, 1993. http://dx.doi.org/10.3133/gp1005.

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2

Maps and seismic profiles showing geology of the inner continental shelf, Cape Ann, Massachusetts to New Hampshire. US Geological Survey, 1987. http://dx.doi.org/10.3133/mf1892.

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3

Bedrock geologic map of Hubbard Brook Experimental Forest and maps of fractures and geology in roadcuts along Interstate 93, Grafton County, New Hampshire. US Geological Survey, 1997. http://dx.doi.org/10.3133/i2562.

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4

Geochemical survey maps of the wildernesses and roadless areas in the White Mountains National Forest, Coos, Grafton, and Carroll counties, New Hampshire. US Geological Survey, 1987. http://dx.doi.org/10.3133/mf1594c.

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5

Isopleth maps showing above-median concentrations of lead and copper in stream-sediment concentrate, Glens Falls 1 degree by 2 degrees Quadrangle, New York, Vermont, and New Hampshire. US Geological Survey, 1992. http://dx.doi.org/10.3133/i2161b.

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6

Isopleth maps showing above-median concentrations of tungsten and tin in stream-sediment concentrate, Glens Falls 1 degree by 2 degrees Quadrangle, New York, Vermont, and New Hampshire. US Geological Survey, 1992. http://dx.doi.org/10.3133/i2161c.

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7

Isopleth maps showing above-median concentrations of barium and strontium in stream-sediment concentrate, Glens Falls 1 degree by 2 degrees Quadrangle, New York, Vermont, and New Hampshire. US Geological Survey, 1992. http://dx.doi.org/10.3133/i2161d.

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8

Isopleth maps showing above-median concentrations of niobium and boron in stream-sediment concentrate, Glens Falls 1 degree x 2 degrees Quadrangle, New York, Vermont, and New Hampshire. US Geological Survey, 1992. http://dx.doi.org/10.3133/i2161e.

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9

Isopleth maps showing above-median concentrations of iron and cobalt in stream-sediment concentrate, Glens Falls 1 degree by 2 degrees Quadrangle, New York, Vermont, and New Hampshire. US Geological Survey, 1992. http://dx.doi.org/10.3133/i2161f.

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10

Tectonic lithofacies, geophysical, and mineral-resource appraisal maps of the Sherbrooke-Lewiston area, Maine, New Hampshire, and Vermont, United States, and Quebec, Canada. US Geological Survey, 1999. http://dx.doi.org/10.3133/i1898e.

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