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Journal articles on the topic 'Hudson'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 August 2024

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1

Zhang, Shunxin, and John F. Riva. "The stratigraphic position and the age of the Ordovician organic-rich intervals in the northern Hudson Bay, Hudson Strait, and Foxe basins—evidence from graptolites." Canadian Journal of Earth Sciences 55, no. 8 (August 2018): 897–904. http://dx.doi.org/10.1139/cjes-2017-0266.

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Graptolites recovered from the organic-rich intervals, previously named the Boas River Formation in the Upper Ordovician succession on Southampton, Akpatok, and southern Baffin islands provide a reliable age assessment for the Upper Ordovician petroleum source rocks in the northern Hudson Bay, Hudson Strait, and Foxe basins. They are characterised by Anticostia lata and Anticostia hudsoni in the lower Red Head Rapids Formation on Southampton Island; Anticostia decipiens and Rectograptus socialis in the lower Foster Bay Formation on Akpatok Island; and Diplacanthograptus spiniferus and Amplexograptus praetypicalis in the lower Amadjuak Formation on southern Baffin Island. These data suggest that the organic-rich intervals in the northern Hudson Bay and Hudson Strait basins can be correlated to the Dicellograptus anceps and Paraorthograptus pacificus zones of the upper Katian, and the horizon in the Foxe Basin to the Diplacanthograptus spiniferus Zone of the lower Katian. The Boas River Formation is not deemed appropriate to use as it occurs as an organic-rich interbed in different stratigraphic units in different basins; therefore, it is suggested to abandon it as a stratigraphic term.

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2

Haile, Alemayehu, and Al Mtenje. "In defence of the autosegmental treatment of nonconcatenative morphology." Journal of Linguistics 24, no. 2 (September 1988): 433–55. http://dx.doi.org/10.1017/s0022226700011853.

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The aim of this paper is to defend the autosegmental account of nonconcatenative morphology originally proposed by McCarthy (1979, 1981), which has been seriously challenged by Hudson (1986). It is argued that an autosegmental analysis of nonconcatenative morphology such as that of Arabic still remains a better alternative than what Hudson proposes. We first present a brief overview of McCarthy's theory of non-concatenative morphology. We then review Hudson's criticisms of such an autosegmental approach to Arabic morphology and we end up by showing why his reanalysis does not constitute a better alternative than the criticized autosegmental account.

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3

Otto, Paul. "The Origins of New Netherland. Interpreting Native American Responses to Henry Hudson's Visit." Itinerario 18, no. 2 (July 1994): 22–39. http://dx.doi.org/10.1017/s0165115300022476.

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When Adriaen van der Donck wrote A Description of the New Netherlands in 1655, he rightly pointed to Henry Hudson's 1609 voyage and discovery as the foundation of Dutch claims to the North American territory. Presumably arguing on the basis of the right of first discovery, he proposed that local Indian lore supported the fact that the Dutch-employed Englishman had been the first to discover and explore the Hudson River. As a settler in New Netherland, Van der Donck had often heard the native inhabitants claim that before Hudson came they had never seen such a thing as a European ship.

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4

Legohérel, Patrick. "Simon Hudson et Louise Hudson, Golf Tourism." Mondes du tourisme, no. 4 (December 1, 2011): 116–17. http://dx.doi.org/10.4000/tourisme.493.

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5

Barr, William. "Shipwrecked on Mansel Island, Hudson Bay: Dr Henry Brietzcke's Arctic health cruise, 1864." Polar Record 28, no. 166 (July 1992): 177–90. http://dx.doi.org/10.1017/s0032247400020647.

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ABSTRACTDuring 664 round trips between London and Hudson Bay from 1670 to 1913,21 of the supply ships of the Hudson's Bay Company were wrecked, mainly in the Bay or in Hudson Strait; a further seven were severely damaged. The year 1864 was remarkable in that out of three ships making the outward voyage to the Bay, two ran aground on Mansel Island only one hour apart. One ship, Prince Arthur, was wrecked and abandoned. The other, Prince of Wales, was refloated and was able to reach York Factory with Prince Arthur's crew on board. There Prince of Wales was condemned; the crews of both ships returned to England on board Ocean Nymph. The events of the double shipwreck, the sojourn of the crew at York Factory, and the voyage home have been reconstructed, mainly on the basis of the journal of the medical officer of the Prince Arthur, the logs of both ships, and other documents in the Hudson's Bay Company Archives.

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6

Kasper, Julia, and Phil Sirvid. "The Treasure of George Vernon Hudson." Biodiversity Information Science and Standards 2 (June 13, 2018): e27006. http://dx.doi.org/10.3897/biss.2.27006.

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George V. Hudson, born 1867 in London, developed a strong interest in nature when he was nine years old and began collecting insects. At the age of 13 he wrote and illustrated his first manuscript on insects. In 1881 Hudson moved to New Zealand, where he worked as a clerk in the post office in Wellington until his retirement in 1919. However, he kept collecting, investigating and describing insects in his spare time, and was determined to present New Zealand’s insect fauna to the general public. He was critical of the formal education system and provided alternative methods of learning through his books. His achievements place him among New Zealand’s distinguished pioneer naturalists. After Hudson’s death in April 1946, his collection of insects, one of the largest and most valuable private collection in New Zealand, was donated to the Dominion Museum with the condition that it remained intact in its nine original cabinets. These are made from kauri and are full of neatly pinned in sects, Hudson invented his own coding system for labelling his specimens. The numbers that refer to each specimen were recorded in three volumes of register books, where he noted details about the samples. These registers are the only way we can understand the collection. However, since Hudson had a very idiosyncratic handwriting and wrote between lines when he ran out of space, his registers are very hard to read. Also, he changed names, deleted numbers of specimens that were given away and reused those numbers. In short, these registers were living documents that changed with the collection. This collection is of immense scientific value and it has been well protected in climate-controlled conditions, although quite inaccessible for many years. Now, the kauri cabinets are secured to shelving units bolted to the floor and a wall. This provides protection against flooding and earthquake hazards. The registers and the specimens in the drawers are part of a digitisation program. All the information on the aging register pages were scanned in high resolution. It is now possible to magnify the writing and transfer the data into a database without touching the vulnerable originals. It is also possible to share the scanned pages with volunteers and experts, who can help deciphering Hudson’s notes. The plan is to make some of the pages available online, as part of a citizen science project.

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7

Cai, Meiqin, Tengchao Huang, Bo Hou, and Ying Guo. "Role of Demyelination Efficiency within Acellular Nerve Scaffolds during Nerve Regeneration across Peripheral Defects." BioMed Research International 2017 (2017): 1–10. http://dx.doi.org/10.1155/2017/4606387.

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Hudson’s optimized chemical processing method is the most commonly used chemical method to prepare acellular nerve scaffolds for the reconstruction of large peripheral nerve defects. However, residual myelin attached to the basal laminar tube has been observed in acellular nerve scaffolds prepared using Hudson’s method. Here, we describe a novel method of producing acellular nerve scaffolds that eliminates residual myelin more effectively than Hudson’s method through the use of various detergent combinations of sulfobetaine-10, sulfobetaine-16, Triton X-200, sodium deoxycholate, and peracetic acid. In addition, the efficacy of this new scaffold in repairing a 1.5 cm defect in the sciatic nerve of rats was examined. The modified method produced a higher degree of demyelination than Hudson’s method, resulting in a minor host immune response in vivo and providing an improved environment for nerve regeneration and, consequently, better functional recovery. A morphological study showed that the number of regenerated axons in the modified group and Hudson group did not differ. However, the autograft and modified groups were more similar in myelin sheath regeneration than the autograft and Hudson groups. These results suggest that the modified method for producing a demyelinated acellular scaffold may aid functional recovery in general after nerve defects.

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8

Pratama, Zamrud Whidas, and Yofi Irvan Vivian. "PERFORMATIVITAS HUDSON PRANANJAYA DALAM PERTUNJUKAN MUSIK." CaLLs (Journal of Culture, Arts, Literature, and Linguistics) 6, no. 2 (December 31, 2020): 197. http://dx.doi.org/10.30872/calls.v6i2.3312.

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Hudson Prananjaya is a singer who has a unique performance that is able to sing in the colors of the voice of men and women like a couple who is a duet. One of the songs he once brought back was the Gethuk song. The purpose of this study is to examine how the performance of a Hudson Prananjaya in exploring the gethuk song so that it has the characteristics of other singers. The theory used in this research is the theory of performativity, Habitus. This study aims to describe how Hudson's performativity in gethuk songs. Data collection is done by (1) literature study, (2) observation, (3) interview, (3) documentation. The stages in analyzing data with (1) data reduction, (2) data presentation, and (3) histography writing (4) conclusion. Clarification of the data was again carried out both to the subject of the study and to other informants. Hudson gained cultural insight in singing because he was accustomed to experimenting in singing. One of the songs that was brought back was Gethuk song. The visual aspect is shown by the concept of two face shows nuances of Javanese customs both makeup and clothes. The results of the transcription and analysis of musical aspects in the introduction section are marked with X sung using the basic tone of Fis Major by taking the first verse of the song yen ing tawang ono latitude. The introduction is sung in a free vocal style without a tempo called the recitative vocal style. Modulation to the Bes Major scale occurs when getting to the Gethuk song starts from the song intro until the song is finished. The gethuk song that Hudson reproduces back to part B (b1 '), (b2'). In the repetition section there is a dialogue technique in singing called unpicth vocal technique.

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9

Burger, Henry G. "Bryan Hudson." Medical Journal of Australia 169, no. 1 (July 1998): 51. http://dx.doi.org/10.5694/j.1326-5377.1998.tb141479.x.

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10

Terán, Ira. "Samantha Hudson." TSQ: Transgender Studies Quarterly 8, no. 4 (November 1, 2021): 557–58. http://dx.doi.org/10.1215/23289252-9311242.

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11

Seaton, Maureen. "Hudson Sonnets." Iowa Review 17, no. 2 (April 1987): 88–90. http://dx.doi.org/10.17077/0021-065x.3518.

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12

Arancet Ruda, María Amelia. "¿Región Hudson?" Letras, no. 87 (September 27, 2023): 171–97. http://dx.doi.org/10.46553/let.87.2023.p171-197.

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En el presente artículo postulamos la existencia de lo que denominamos Región Hudson. Para ello elegimos el nombre de región (Molina y Varela; Heredia), pero enriquecemos el concepto con lo que regionalidad (Arendt) y biorregión (McGinnis et alii) tienen para aportar. A su vez, nuestra mirada sobre esta región es eco, de acuerdo con algunos de los teóricos del amplio espectro de la ecocrítica, especialmente Mathews, Naess y Fukuoka. Esta elección parece el devenir natural para considerar un autor como William Henry Hudson, preocupado por el conservacionismo natural desde el siglo XIX. Así, damos notas de lo que consideraremos región; tomaremos para la región Hudson los elementos cognitivos indicados para ello por Mariana N. Saua y finalmente veremos cómo se concreta esta región. No es una propuesta que parte de lo abstracto, sino de constatar que en la zona del Río de la Plata son las muchas producciones que, de distintas maneras, se ubican en la estela de Hudson en cuanto a: el amor por la naturaleza, su percepción como vivencia íntima y, luego, la puesta en discurso. Aquí, además de considerar su Allá lejos y hace tiempo (1918), añadimos las obras Allá en lo verde Hudson (2012), de Arnaldo Calveyra; Libro de horas (2015), de Laura Forchetti; y Ornitología para principiantes (2018), de Daniel Dellazuana.

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13

Stravers, Jay A., Gifford H. Miller, and Darrell S. Kaufman. "Late glacial ice margins and deglacial chronology for southeastern Baffin Island and Hudson Strait, eastern Canadian Arctic." Canadian Journal of Earth Sciences 29, no. 5 (May 1, 1992): 1000–1017. http://dx.doi.org/10.1139/e92-083.

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Radiocarbon dates from marine piston cores and from onshore raised marine stratigraphic sections in the Hudson Strait region were used to reconstruct deglacial isochrons for 9900, 9500, 8800–8500, and 8000 BP. At the culmination of the Gold Cove readvance (9900 BP), Labrador–Ungava ice flowed northeastward across Hudson Strait and outer Frobisher Bay and stood for the last time on the Baffin Island continental shelf. Subsequent retreat by calving was rapid and profound, opening the entire Hudson Strait marine trough by 9500 BP. At this time, ice dispersal from Foxe Basin, Labrador–Ungava, and local ice on Meta Incognita Peninsula supported tidewater margins along much of the coastline, with the exception of northernmost Ungava Peninsula, where the ice margin stabilized onshore. This onshore margin remained in place throughout the Cockburn Substage while a major northeastward readvance of Ungava Bay ice (the Noble Inlet readvance from 8800 to 8500 BP) crossed outer Hudson Strait, grounding on the Hudson Strait sill and the south coast of Meta Incognita Peninsula. Sedimentation continued in an enclosed basin in western Hudson Strait, but marine circulation was prohibited by the ice dam, and upper water column salinities became too low to support a marine molluscan fauna. Ungava Bay ice was not thick enough to sustain flow across eastern Hudson Strait, and rising sea levels soon destroyed the Noble Inlet ice dam. By 8300 BP normal marine waters were circulating in eastern Hudson Strait, followed shortly thereafter (at 8100 BP) by the deglaciation of western Hudson Strait and Hudson Bay.

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14

Gray, James, Bernard Lauriol, Denis Bruneau, and Jean Ricard. "Postglacial emergence of Ungava Peninsula, and its relationship to glacial history." Canadian Journal of Earth Sciences 30, no. 8 (August 1, 1993): 1676–96. http://dx.doi.org/10.1139/e93-147.

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A series of 178 radiocarbon dates, of late glacial and postglacial age, from raised marine terraces on the Hudson Strait, Hudson Bay, and Ungava Bay coasts, permit a new synthesis of deglaciation history, postglacial emergence, and glacio-isostatic recovery of the Ungava Peninsula. Marine limits show three local highs, related to centres of ice loading: east of Hudson Bay; southwest of Ungava Bay, and in western Hudson Strait. Eastward extension of the latter to Cap de Nouvelle-France is attributed to early deglaciation. Emergence curves are presented from sites in (1) Hudson Strait ice-free prior to 9 ka; (2) Hudson Strait; (3) Hudson Bay; and (4) Ungava Bay liberated by Ungava ice between 8 and 6 ka. A sigmoidal pattern for the first group, with slow initial emergence, contrasts markedly with a pattern of rapid deceleration of emergence for the other groups. These differences are attributed to variations in rates of ice sheet unloading, immediately after coastal deglaciation. A stable onshore ice margin kept the northeastern tip of Ungava isostatically depressed, from initial deglaciation until 7 ka, whereas other mainland coasts were only liberated by retreat of the ice margin during a final phase of rapid thinning of the continental ice sheet. Isobases on emergence since 6.5, 5, and 2 ka, derived from marine and glacial lake shoreline data, indicate maximum ice loading centres in eastern Hudson Bay and in central Quebec–Labrador, with an extension northwards towards Ungava Bay. An uplift rate of 14 mm/year since 2 ka for Inukjuak on the Hudson Bay coast is compatible with very high tide gauge values. A downward gradient of 6.5 ka isobases in a northeasterly direction from southeastern Ungava towards present sea level on southern Resolution Island at the mouth of Hudson Strait suggests that Ungava Bay, despite late occupation by glacial ice, was probably not a major loading centre.

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15

Stewart, Robert E. A. "Size-at-age relationships as discriminators of white whale (Delphinapterus leucas) stocks in the eastern Canadian Arctic." Meddelelser om Grønland. Bioscience 39 (April 22, 1994): 217–25. http://dx.doi.org/10.7146/mogbiosci.v39.142552.

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White whales harvested by Inuit at Arviat on western Hudson Bay, Pangnirtung on Cumberland Sound and Grise Fiord on the north side of Jones Sound were sampled for analysis of size and age in 1984-87. The sampling sites are thought to represent western Hudson Bay, Southeast Baffin and High Arctic stocks of white whales, respectively. Males were longer than females at all locations. White whales from western Hudson Bay were significantly shorter as adults than white whales from the other two locations. Analysis of published data showed that eastern Hudson Bay white whales are also significantly smaller than Cumberland Sound whales. Differences in asymptotic length between whales from Cumberland Sound and Jones Sound, and between whales from eastern and western Hudson Bay, were not significant.

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16

Kerwin, Michael W. "A Regional Stratigraphic Isochron (ca. 8000 14C yr B.P.) from Final Deglaciation of Hudson Strait." Quaternary Research 46, no. 2 (September 1996): 89–98. http://dx.doi.org/10.1006/qres.1996.0049.

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Sedimentologic, rock-magnetic, and X-ray fluorescence data from two marine sediment cores in Hudson Strait suggest that a red, hematite-rich clay layer was deposited throughout the strait during the final collapse of the Laurentide Ice Sheet in the vicinity of northern Hudson Bay and western Hudson Strait. This layer, which can be recognized by its reddish-pink color (10YR6/2 to 5YR4/2) and relatively high-hematite proportions (low magnetic susceptibility and magnetite-to-hematite ratio), is dated from 8000 to 7900 14C yr B.P. at both ends of the strait. The Dubawnt Group, a Proterozoic bedrock unit in northern Hudson Bay, is the most likely source of this stratigraphic isochron. In eastern Hudson strait, the recognition of this red unit and other distal glaciomarine sediments from 8400 to 7900 14C yr B.P. indicates that little sediment from the nearby Labrador Dome reached eastern Hudson Strait during this 500-yr interval. This time interval immediately postdates the Noble Inlet advance, a northward flow of Labrador ice across eastern Hudson Strait onto southern Baffin Island from ca. 8900 to 8400 14C yr B.P. One explanation for the lack of Labrador sediments is that the northern margin of the Labrador dome was cold-based for up to 500 yr following the Noble Inlet advance.

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17

Miller, Gifford H., Paul J. Hearty, and Jay A. Stravers. "Ice-Sheet Dynamics and Glacial History of Southeasternmost Baffin Island and Outermost Hudson Strait." Quaternary Research 30, no. 2 (September 1988): 116–36. http://dx.doi.org/10.1016/0033-5894(88)90018-x.

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Southeasternmost Baffin Island is mantled by Hudson Strait drift; it contains abundant limestone erratics and 20 to 50% carbonate in the matrix. To the northwest, it is replaced by drift dominated by locally derived rock of the Canadian Shield. The sense and orientation of ice-erosional features demonstrate that Hudson Strait drift is associated with northeasterly ice flow that crossed the tip of Meta Incognita Peninsula; local drift, associated with ice flow S10°W along the Hudson Strait coast, was derived from a dispersal center on the peninsula. Erratic lithologies contained in the Hudson Strait drift indicate a Labradorean provenance. Large-scale bedrock molding and the distribution of cirques indicate NE-flowing ice has been dominant throughout the middle and late Quaternary. Radiocarbon dates of in situ shells confirm that deglaciation began more than 11,000 yr ago, with the Frobisher Bay coast becoming ice free by 9300 yr ago. Five dates from Hudson Strait suggest that the strait was deglaciated before 9000 yr BP. However, ice from the Labradorean Sector recrossed Hudson Strait during the Cockburn Substage, about 8500 yr ago, damming drainage from the west. Final retreat of Labradorean ice from Baffin Island was complete by 8000 yr ago, at which time the sea was able to penetrate Hudson Bay.

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18

Bracamonte, Jorge. "Literatura argentina y extranjería: variaciones Piglia sobre Hudson." Letras, no. 87 (September 27, 2023): 156–70. http://dx.doi.org/10.46553/let.87.2023.p156-170.

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Los vínculos construidos por la poética de Ricardo Piglia con la figura, trayectoria y obra de William Hudson recorren distintas etapas, diferentes variaciones. Respecto a Hudson, resulta decisiva para Piglia la valoración que Ezequiel Martínez Estrada hace de la obra y trayectoria de Hudson. Ello se detecta desde los años de formación del joven escritor Piglia, durante la década de 1950. Luego, durante las décadas de 1960 y 1970, el gradual y radical posicionamiento teórico y político-literario de Piglia lo llevará a considerar en algún momento la figura de Hudson como la de un extranjero de notable obra, pero en definitiva exótico y que permanece en una mirada colonizada respecto a la cultura argentina. Finalmente, Piglia revaloriza al Hudson lector y escritor, clave para las literaturas y culturas argentina y anglosajona, quien también es un crítico radical del capitalismo. Este ensayo interroga los matices de esos diferentes momentos.

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19

Hudson, Georgia. "Interview: Georgia Hudson." Alphaville: journal of film and screen media, no. 25 (August 30, 2023): 123–28. http://dx.doi.org/10.33178/alpha.25.09.

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Georgia Hudson is a director and artist, born and raised in London. Georgia established her career through making music videos such as Pink’s What About Us (2017). In 2019 she was awarded Director of the Year by Shots for her body of work. Recognised for her emotion-driven storytelling, Hudson has made award-winning commercial films for Nike, Beats, BBC, Zalando, Budweiser and O2 amongst many others. She has collaborated with a range of musicians including Loyle Carner, Tom Misch, MØ, Jorja Smith, and Lenny Kravitz. Her short film Temper and poetry book Orange Eyes were released in 2021. Hudson is represented by production company Park Pictures in the UK and USA.

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20

Gordon, Donald C. "Remembering Hudson-70." Proceedings of the Nova Scotian Institute of Science (NSIS) 51, no. 1 (February 4, 2021): 9. http://dx.doi.org/10.15273/pnsis.v51i1.10732.

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Hudson-70 was the last big multidisciplinary global oceanographic expedition. Organized by the Bedford Institute of Oceanography (BIO), based in Nova Scotia, this epic eleven-month voyage lasted from November 1969 to October 1970, involved 128 scientists from five countries, and traversed five oceans. Enroute, the CSS Hudson steamed 56,000 nautical miles and became the first ship to circumnavigate the Americas. A huge amount of new oceanographic information in all disciplines was collected in environments ranging from tropical to polar. Major highlights are summarized. General overviews of the expedition were published in three books and the results of individual studies were reported in over 50 scientific publications. Hudson-70 was a major Canadian oceanographic accomplishment, truly worthy of celebrating fifty years later.

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21

Goodpaster, Kenneth E., and Robert G. Kennedy. "Dayton Hudson Corporation." Proceedings of the International Association for Business and Society 2 (1991): 257–82. http://dx.doi.org/10.5840/iabsproc1991210.

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22

Rhys, Guto. "Hudson, The Picts." Scottish Historical Review 97, no. 1 (April 2018): 119–21. http://dx.doi.org/10.3366/shr.2018.0355.

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23

Mahony, Christina Hunt, Derek Mahon, and Ciaran Carson. "The Hudson Letter." Canadian Journal of Irish Studies 25, no. 1/2 (1999): 539. http://dx.doi.org/10.2307/25515296.

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24

Rathmann, Andrew, and Derek Mahon. "The Hudson Letter." Chicago Review 42, no. 2 (1996): 100. http://dx.doi.org/10.2307/25304120.

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25

Harrison, R. T. "Edward Gordon Hudson." Medical Journal of Australia 151, no. 9 (November 1989): 530. http://dx.doi.org/10.5694/j.1326-5377.1989.tb128508.x.

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26

Brown, Ashley, and Derek Mahon. "The Hudson Letter." World Literature Today 72, no. 1 (1998): 139. http://dx.doi.org/10.2307/40153614.

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27

Thistlewood, David. "Obituary: Tom Hudson." Journal of Art & Design Education 17, no. 2 (May 1998): 115–16. http://dx.doi.org/10.1111/1468-5949.00114.

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28

Dorcely, Marie-Ovide Gina. "Hudson River School." Callaloo 30, no. 1 (2007): 118. http://dx.doi.org/10.1353/cal.2007.0119.

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29

Hubner, Peter. "Norah Marion Hudson." BMJ 334, no. 7601 (May 10, 2007): 1011.3–1011. http://dx.doi.org/10.1136/bmj.39199.673206.be.

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30

Nash, Andrew. "Remembering Peter Hudson." Transformation: Critical Perspectives on Southern Africa 104, no. 1 (2020): 135–45. http://dx.doi.org/10.1353/trn.2020.0039.

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31

Han, Jeffrey, Michael Martello, and Kenneth Wright. "Bridging the Hudson." Civil Engineering Magazine Archive 89, no. 9 (October 2019): 54–61. http://dx.doi.org/10.1061/ciegag.0001420.

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32

Ethridge, Robbie. "Remembering Charles Hudson." Native South 7, no. 1 (2014): 146–49. http://dx.doi.org/10.1353/nso.2014.0003.

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33

White, HC. "Jack Hudson Francis." Australian Veterinary Journal 76, no. 5 (May 1998): 367. http://dx.doi.org/10.1111/j.1751-0813.1998.tb12374.x.

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34

Bays, Timothy. "Hudson on Receptacles." Australasian Journal of Philosophy 81, no. 4 (December 2003): 569–72. http://dx.doi.org/10.1080/713659763.

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35

Arlow, Ruth, and Will Adam. "Re Hudson (deceased)." Ecclesiastical Law Journal 11, no. 3 (August 6, 2009): 363–64. http://dx.doi.org/10.1017/s0956618x09990251.

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36

Busciglio-Ritter, Thomas. "Paris-on-Hudson." Athanor 37 (December 3, 2019): 59–66. http://dx.doi.org/10.33009/fsu_athanor116676.

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In 1969, a curious picture entered the collections of the Metropolitan Museum of Art, in New York City, as part of a major bequest by American banker Robert Lehman (1891-1969). Identified as a Hudson River Scene, the painting, undated and unsigned, depicts an idyllic river landscape, surrounded by green hills, indeed reminiscent of the Hudson River School. Yet the attribution devised by the museum for might appear curious at first glance, as it does not rule out the possibility of a work produced by a little-known French painter named Victor de Grailly. Born in Paris in 1804, Grailly died in the same city in 1887. Mentioned in several museum collections, his pictures constitute a debatable body of work to this day. But if only a few biographical elements have been saved about the artist, the crunch of the debate lies elsewhere.

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37

Martin, Cynthia. "Dr. Alan Hudson." Healthcare Quarterly 5, no. 2 (December 15, 2001): 72–76. http://dx.doi.org/10.12927/hcq..16522.

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38

PARSONS, JOSH. "Hudson on Location." Philosophy and Phenomenological Research 76, no. 2 (March 2008): 427–35. http://dx.doi.org/10.1111/j.1933-1592.2007.00143.x.

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39

Howard, Jason Kyle. "Patricia L. Hudson." Appalachian Review 51, no. 1-2 (January 2023): 70–80. http://dx.doi.org/10.1353/aph.2023.a926418.

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Johnson, R. G., and S. E. Lauritzen. "Hudson Bay-Hudson Strait jökulhlaups and Heinrich events: a hypothesis." Palaeogeography, Palaeoclimatology, Palaeoecology 117, no. 1-2 (August 1995): 123–37. http://dx.doi.org/10.1016/0031-0182(94)00120-w.

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Leung, Andrew C. W., William A. Gough, and Ken A. Butler. "Changes in Fog, Ice Fog, and Low Visibility in the Hudson Bay Region: Impacts on Aviation." Atmosphere 11, no. 2 (February 10, 2020): 186. http://dx.doi.org/10.3390/atmos11020186.

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Fog and low visibility present a natural hazard for aviation in the Hudson Bay region. Sixteen communities on the eastern and western shores of Hudson and James Bays, Canada, were selected for fog, ice fog, and low visibility statistical analyses for a range of 21 to 62 year time series. Both fog hours and ice fog hours were found to be in general decline, with some locations experiencing statistically significant declines. Spatial asymmetries for fog and ice fog were observed among the various areas within the Hudson Bay region. The more northerly locations in this study experienced statistically significant declines in fog hours while the southerly locations’ declines were not significant. Fog was significantly declining in some western Hudson Bay locations during spring and fall and in James Bay during winter and summer, but minimal trends were observed in eastern Hudson Bay. For ice fog hours, all of the locations in the western shore of Hudson Bay experienced a significant decline in winter while only one-third of the locations in eastern shores were found to be declining significantly during winter. Blowing snow, snow, ice and fog were the leading causes for reduced and low visibilities at the majority of the locations. Other factors such as rain contributed a minor role to low visibility.

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Pace, Michael L., Stuart E. G. Findlay, and David Lints. "Variance in Zooplankton Samples: Evaluation of a Predictive Model." Canadian Journal of Fisheries and Aquatic Sciences 48, no. 1 (January 1, 1991): 146–51. http://dx.doi.org/10.1139/f91-020.

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We derived mean-variance relationships for zooplankton samples taken in the Hudson River and a series of Quebec lakes. Hudson River and Quebec lakes data were used to test a published model by comparing observed with predicted variance. In addition, we examined patterns of mean-variance relations (1) at higher levels of taxonomic organization, (2) between riverine and open water systems, and (3) between taxa common to the Hudson River and Quebec lakes data sets. There was an excellent correspondence between observed variance for the Hudson River and Quebec lakes data sets and the variance predicted using the model. Mean-variance relationships for higher taxa (cladocerans, copepods, rotifers) were similar to the general models. Zooplankton variance in the Hudson River was comparable with patterns observed in lentic systems contrary to our initial hypothesis that riverine zooplankton, because of rapid turbulent mixing, would have lower variance. Mean-variance relationships for taxa common to the Hudson River and Quebec lakes were comparable in three of six cases, but for the remaining three cases, regression intercepts were marginally different (P = 0.03–0.05) between systems. We conclude that zooplankton mean-variance relationships are highly consistent and predictable for a variety of aquatic systems and levels of taxonomic organization.

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Parthasarathy, K. R. "On Some Markov Processes Arising from the Eyre-Hudson Super Lie Algebra Representations." Infinite Dimensional Analysis, Quantum Probability and Related Topics 01, no. 03 (July 1998): 485–98. http://dx.doi.org/10.1142/s0219025798000260.

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It is well-known3,5 that Brownian motion and Poisson process arise naturally from the canonical commutation relations (CCR) of free field operators in a boson Fock space. Eyre and Hudson2 have recently shown how to construct fields of operators in a boson Fock space obeying super Lie commutation relations. We establish the essential self-adjointness of their real and imaginary parts on the domain ∊, the linear manifold generated by all the exponential (coherent) vectors and determine a family of Markov processes which they give rise to in a natural manner. These Markov processes yield examples of Evans–Hudson flows3,5 and Azéma-like martingales.1,4,6

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Bilodeau, Guy, Anne de Vernal, Claude Hillaire-Marcel, and Heiner Josenhans. "Postglacial paleoceanography of Hudson Bay: stratigraphic, microfaunal, and palynological evidence." Canadian Journal of Earth Sciences 27, no. 7 (July 1, 1990): 946–63. http://dx.doi.org/10.1139/e90-098.

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Cores containing representative sequences of postglacial sediments in northern and southern Hudson Bay were analyzed for their microfaunal (foraminifers and ostracods) and palynological (dinocysts, pollen, and spores) content in order to reconstruct the evolution of environments since the last glaciation.In southern Hudson Bay, the marine invasion of the Tyrrell Sea at ca. 8000 BP, following the Lake Ojibway episode, was accompanied by the development of an Arctic-type microflora and microfauna indicative of a dense seasonal sea-ice cover and stratified water masses. Shortly after 8000 BP, the establishment of subarctic conditions in surface waters was accompanied by more intense homogenization of water masses. Subarctic conditions have persisted throughout most of the postglacial interval despite a recent surface-water cooling.In northern Hudson Bay, micropaleontological and lithological data reveal a succession of proximal to distal glaciomarine environments characterized by low biogenic productivity, harsh Arctic conditions, and stratified water masses. An increase in dinocyst abundance and diversity, after 6000 BP, indicates the establishment of cool subarctic conditions in surface waters, while foraminifer assemblages suggest intensified mixing of water masses.The micropaleontological records of northern and southern Hudson Bay reveal a strong latitudinal gradient in biogenic productivity and water mass characteristics throughout the postglacial interval. "Interglacial" conditions, established in southern Hudson Bay very shortly after it was invaded by the sea, seem to have occurred much later in northern Hudson Bay.

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Webb, D. J. "On the tides and resonances of Hudson Bay and Hudson Strait." Ocean Science 10, no. 3 (May 28, 2014): 411–26. http://dx.doi.org/10.5194/os-10-411-2014.

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Abstract. The resonances of Hudson Bay, Foxe Basin and Hudson Strait are investigated using a linear shallow water numerical model. The region is of particular interest because it is the most important region of the world ocean for dissipating tidal energy. The model shows that the semi-diurnal tides of the region are dominated by four nearby overlapping resonances. It shows that these not only affect Ungava Bay, a region of extreme tidal range, but they also extend far into Foxe Basin and Hudson Bay and appear to be affected by the geometry of those regions. The results also indicate that it is the four resonances acting together which make the region such an important area for dissipating tidal energy.

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Webb, D. J. "On the tides and resonances of Hudson Bay and Hudson Strait." Ocean Science Discussions 10, no. 6 (November 5, 2013): 2053–83. http://dx.doi.org/10.5194/osd-10-2053-2013.

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Abstract. The resonances of Hudson Bay, Foxe Basin and Hudson Strait are investigated using a~linear shallow water numerical model. The region is of particular interest because it is the most important region of the world ocean for dissipating tidal energy. The model shows that the semi-diurnal tides of the region are dominated by four nearby overlapping resonances. It shows that these not only affect Ungava Bay, a region of extreme tidal range, but they also extend far into Foxe Basin and Hudson Bay and appear to be affected by the geometry of those regions. The results also indicate that it is the four resonances acting together which make the region such an important area for dissipating tidal energy.

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Seeger, Pete, and Linda C. Forbes. "Possibility and Hope: Getting from Here to There." Monthly Review 66, no. 8 (January 6, 2015): 30. http://dx.doi.org/10.14452/mr-066-08-2015-01_6.

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Pete Seeger is an environmental advocate who understands the transforming power of immersion in nature. However, his desire to restore his cherished Hudson River posed a monumental challenge in the 1960s. The Hudson River, once so majestic that it inspired the Hudson River School painters, had become a sewer for the communities and commercial industries that populated its shoreline. Seeger’s approach to reversing the degradation of the Hudson River involved a unique form of advocacy and organizing. He envisioned healing the Hudson through immersion. His approach involved bringing people back to the river aboard a 106-foot replica of a Hudson River sloop (a single-masted sailboat), one that resembled the boats that traversed the Hudson in centuries past. By 1969, with Seeger as the driving force behind its creation, the sloop Clearwater was constructed and launched. It still sails today and serves as an inspiring symbol of citizen activism on behalf of the natural environment.<p class="mrlink">This article can also be found at the <a href="http://monthlyreview.org/index/volume-66-number-7" title="Vol. 66, No. 7: January 2015" target="_blank"><em>Monthly Review</em> website</a>, where most recent articles are published in full.</p><p class="mrpurchaselink"><a href="http://monthlyreview.org/index/volume-66-number-7" title="Vol. 66, No. 7: January 2015" target="_self">Click here to purchase a PDF version of this article at the <em>Monthly Review</em> website.</a></p>

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Tivy, Adrienne, Stephen E. L. Howell, Bea Alt, John J. Yackel, and Thomas Carrieres. "Origins and Levels of Seasonal Forecast Skill for Sea Ice in Hudson Bay Using Canonical Correlation Analysis." Journal of Climate 24, no. 5 (March 1, 2011): 1378–95. http://dx.doi.org/10.1175/2010jcli3527.1.

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Abstract Canonical correlation analysis (CCA) is used to estimate the levels and sources of seasonal forecast skill for July ice concentration in Hudson Bay over the 1971–2005 period. July is an important transition month in the seasonal cycle of sea ice in Hudson Bay because it is the month when the sea ice clears enough to allow the first passage of ships to the Port of Churchill. Sea surface temperature (quasi global, North Atlantic, and North Pacific), Northern Hemisphere 500-mb geopotential height (z500), sea level pressure (SLP), and regional surface air temperature (SAT) are tested as predictors at 3-, 6-, and 9-month lead times. The model with the highest skill has three predictors—fall North Atlantic SST, fall z500, and fall SAT—and significant tercile forecast skill covering 61% of the Hudson Bay region. The highest skill for a single-predictor model is from fall North Atlantic SST (6-month lead). Fall SST explains 69% of the variance in July ice concentration in Hudson Bay and a possible atmospheric link that accounts for the lagged relationship is presented. CCA diagnostics suggest that changes in the subpolar North Atlantic gyre and the Atlantic multidecadal oscillation (AMO), reflected in sea surface temperature, precedes a deepening/weakening of the winter upper-air ridge northwest of Hudson Bay. Changes in the height of the ridge are reflected in the strength of the winter northwesterly winds over Hudson Bay that have a direct impact on the winter ice thickness distribution; anomalies in winter ice severity are later reflected in the pattern and timing of spring breakup. July ice concentration in Hudson Bay has declined by approximately 20% per decade between 1979 and 2007, and the hypothesized link to the AMO may help explain this significant loss of ice.

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Maranguello, Carolina. "Conservar el mundo más maravilloso: William H. Hudson en Libro de horas de Laura Forchetti." Káñina 45, no. 3 (November 3, 2021): 35–56. http://dx.doi.org/10.15517/rk.v45i3.48968.

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En 2017 se publicó Libro de horas, poemario en el que Laura Forchetti recupera la figura y la obra del escritor inglés William Henry Hudson, quién pasó su infancia y juventud en Argentina y particularizó el paisaje nacional a partir de su singular observación. Teniendo en cuenta la especial relación que Hudson estableció en varios de sus trabajos entre autobiografía, discurso naturalista y contemplación poética de la naturaleza, el objetivo de este artículo será considerar la recepción contemporánea e íntima de Hudson y el “Deseo de escritura” (Barthes, 2005) que produce su lectura, presentes en varios escritores de literatura argentina y que Forchetti figura de un modo particular. Como se verá, dialogando con su obra y con las memorias de infancia de Hudson, su poemario indaga distintas formas escriturales (el diario íntimo, el herbario, el Libro de Horas medieval, entre otras), a partir de la precaria potencia de la mirada. Modela, en relación a ellas, diversas declinaciones temporales entre las que la difusa religiosidad animista de Hudson será fundamental. Por último, abriendo su propia escritura a los deseos expresados por el escritor inglés en Allá lejos y hace tiempo, los reescribe, escenificando su muerte en la pampa.

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Parks, E. K., A. E. Derocher, and N. J. Lunn. "Seasonal and annual movement patterns of polar bears on the sea ice of Hudson Bay." Canadian Journal of Zoology 84, no. 9 (September 2006): 1281–94. http://dx.doi.org/10.1139/z06-115.

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Polar bears ( Ursus maritimus Phipps, 1774) move thousands of kilometres over sea ice searching for mates and hunting for seals, which are their primary prey. Recently, decreased sea ice extent and earlier ice break-up have been linked to shifts in seal distribution and abundance and to declines in polar bear condition and numbers in the western Hudson Bay polar bear population. We used geographic positioning system and satellite collars deployed between 1991 and 2004 to quantify movement patterns of adult female polar bears on the sea ice of Hudson Bay in relation to reproductive class and temporal variations in sea ice patterns. We tested whether reproductive status and season affected movement and whether temporal changes in movement were correlated with temporal changes in sea ice patterns in Hudson Bay. Movement patterns were not dependent on reproductive status but did change significantly with season. Annual distances moved and areas covered by bears in Hudson Bay have decreased since 1991, which suggests that measured declines in bear condition and numbers are due to reduced prey intake as opposed to increased energy output. These declines in bear movement are correlated with progressively earlier ice break-up in western Hudson Bay.

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