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1

Haskins, Jacqueline. "Fairweather Gods." Iowa Review 46, no. 1 (March 2016): 35–48. http://dx.doi.org/10.17077/0021-065x.7684.

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2

O'hara, James J. "The New Gallus and the Alternae Voces of Propertius 1.10.10." Classical Quarterly 39, no. 2 (December 1989): 561–62. http://dx.doi.org/10.1017/s0009838800037629.

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In CQ 34 (1984), 167–74, Janet Fairweather makes the interesting suggestion that the elegiacs by Gallus on the Qasr Ibrim papyrus should be understood as ‘a fragment of an amoebaean song-contest’. This hypothesis, as she notes, might explain why the papyrus' quatrains are set apart by spaces and by an odd type of symbol, and treat ‘separate, indeed discrepant, topics’, yet show ‘unmistakable verbal and thematic connections’. Fairweather's discussion is thorough, but overlooks one small piece of evidence for Gallan amoebaean verse.
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3

Buchner, Howard. "Fairweather at Trinity." Toronto Journal of Theology 3, no. 1 (March 1987): 138–41. http://dx.doi.org/10.3138/tjt.3.1.138.

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4

Witter, Robert C., Adrian M. Bender, Katherine M. Scharer, Christopher B. DuRoss, Peter J. Haeussler, and Richard O. Lease. "Geomorphic expression and slip rate of the Fairweather fault, southeast Alaska, and evidence for predecessors of the 1958 rupture." Geosphere 17, no. 3 (May 6, 2021): 711–38. http://dx.doi.org/10.1130/ges02299.1.

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Abstract Active traces of the southern Fairweather fault were revealed by light detection and ranging (lidar) and show evidence for transpressional deformation between North America and the Yakutat block in southeast Alaska. We map the Holocene geomorphic expression of tectonic deformation along the southern 30 km of the Fairweather fault, which ruptured in the 1958 moment magnitude 7.8 earthquake. Digital maps of surficial geology, geomorphology, and active faults illustrate both strike-slip and dip-slip deformation styles within a 10°–30° double restraining bend where the southern Fairweather fault steps offshore to the Queen Charlotte fault. We measure offset landforms along the fault and calibrate legacy 14C data to reassess the rate of Holocene strike-slip motion (≥49 mm/yr), which corroborates published estimates that place most of the plate boundary motion on the Fairweather fault. Our slip-rate estimates allow a component of oblique-reverse motion to be accommodated by contractional structures west of the Fairweather fault consistent with geodetic block models. Stratigraphic and structural relations in hand-dug excavations across two active fault strands provide an incomplete paleoseismic record including evidence for up to six surface ruptures in the past 5600 years, and at least two to four events in the past 810 years. The incomplete record suggests an earthquake recurrence interval of ≥270 years—much longer than intervals <100 years implied by published slip rates and expected earthquake displacements. Our paleoseismic observations and map of active traces of the southern Fairweather fault illustrate the complexity of transpressional deformation and seismic potential along one of Earth's fastest strike-slip plate boundaries.
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5

Enkelmann, Eva, and Sarah Falkowski. "Deformation between the highly oblique Yakutat–North American plate boundary and the Eastern Denali fault." Geosphere 17, no. 6 (October 27, 2021): 2123–43. http://dx.doi.org/10.1130/ges02410.1.

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Abstract This study investigates the spatial and temporal pattern of rock exhumation inboard of the highly oblique Yakutat–North American plate boundary. We aim to quantify how far deformation is transferred inboard of the Fairweather transform plate boundary and across the Eastern Denali fault. We present new detrital apatite and zircon fission track data from 27 modern drainages collected on both sides of the Eastern Denali fault and from the Alsek and Tatshenshini River catchments that drain the mountainous region between the Fairweather fault and the Eastern Denali fault. By integrating our data with published bedrock and detrital geochronology and thermochronology, we show that exhumation reaches much farther inboard (>100 km) of the Fairweather fault than farther north in the St. Elias syntaxial region (<30 km). This suggests that the entire corridor between the Fairweather and Eastern Denali faults exhumed since mid-Miocene time. The Eastern Denali fault appears to be the backstop, and late Cenozoic exhumation northeast of the fault is very limited.
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6

Bermingham, Charles, Christopher F. Manlick, and William Ming Liu. "Mental health, permanent housing, and peer support through community living in the Fairweather Lodge: implementation through collaboration." Housing, Care and Support 18, no. 1 (March 16, 2015): 26–30. http://dx.doi.org/10.1108/hcs-02-2015-0002.

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Purpose – The purpose of this paper is to explain the history of the Fairweather Lodge Program, its utility, the development of one program in a small Midwestern city, the role of psychology, and the importance of disseminating information about the program to combat homelessness. Design/methodology/approach – This paper takes a short case study approach to describing the evolution of a peer support-based housing program for individuals with serious mental illness and a history of homelessness. Findings – The Fairweather Lodge facilitates peer support, community engagement, stable housing, and work engagement in those struggling with mental illness and homelessness. Originality/value – The Fairweather Lodge Program is a program intended to support the mental health and employment needs of individuals with severe mental illness who are at increased risk of homelessness. Housing alone often does not address the complex needs of chronically homeless individuals.
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7

Fennell, William. "Eugene Fairweather as Ecumenical Partner." Toronto Journal of Theology 3, no. 1 (March 1987): 134–37. http://dx.doi.org/10.3138/tjt.3.1.134.

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8

Aiton, Jim, Eric Flitney, Bob Pitman, and Nick Simmons. "Obituary: Joseph Fairweather Lamb FRSE." Physiology News, Winter 2015 (January 1, 2016): 40–41. http://dx.doi.org/10.36866/pn.101.40.

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9

Roberts, Claire. "Ian Fairweather: The Drunken Buddha." Australian and New Zealand Journal of Art 18, no. 2 (July 3, 2018): 224–41. http://dx.doi.org/10.1080/14434318.2018.1516494.

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10

Lofft, Jonathan S. "‘Two Young Ladies in Connection with a Certain School:’ The Watson-Ketcheson Affair of 1952–53 and the Remains of Eugene R. Fairweather." Journal of Anglican Studies 16, no. 1 (March 23, 2018): 7–22. http://dx.doi.org/10.1017/s1740355318000049.

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AbstractTwo young teachers posted at an Indian Residential School in Saskatchewan, Canada, sought to act as whistleblowers regarding abuse there in 1952–53. Theologian Eugene R. Fairweather of Trinity College, Toronto, acted as their advocate and spiritual advisor. A significant correspondence, mostly purged from the official record, considered the reports of the whistleblowers, their fate, and the fraught place of the Residential Schools in Canadian Anglicanism in the decades before the era of Truth and Reconciliation. This article examines the relevant correspondence, retained only in the archival remains of Fairweather at Trinity. The correspondence, which adds to existing narratives of Anglican complicity in and responses to abuse at the Schools, suggests that future research must scrutinize official as well as previously overlooked sources of information, particularly the archival repositories of universities and theological schools, in search of the truth.
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11

Heaney, Robert P., M. Susan Dowell, Karen Rafferty, and June Bierman. "Reply to B Teucher and SJ Fairweather-Tait." American Journal of Clinical Nutrition 73, no. 1 (January 1, 2001): 128–29. http://dx.doi.org/10.1093/ajcn/73.1.128a.

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12

Abu Mansor, N., A. K. Zulkifle, N. Alias, M. K. Hasan, and M. J. N. Boyce. "The Higher Accuracy Fourth-Order IADE Algorithm." Journal of Applied Mathematics 2013 (2013): 1–13. http://dx.doi.org/10.1155/2013/236548.

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This study develops the novel fourth-order iterative alternating decomposition explicit (IADE) method of Mitchell and Fairweather (IADEMF4) algorithm for the solution of the one-dimensional linear heat equation with Dirichlet boundary conditions. The higher-order finite difference scheme is developed by representing the spatial derivative in the heat equation with the fourth-order finite difference Crank-Nicolson approximation. This leads to the formation of pentadiagonal matrices in the systems of linear equations. The algorithm also employs the higher accuracy of the Mitchell and Fairweather variant. Despite the scheme’s higher computational complexity, experimental results show that it is not only capable of enhancing the accuracy of the original corresponding method of second-order (IADEMF2), but its solutions are also in very much agreement with the exact solutions. Besides, it is unconditionally stable and has proven to be convergent. The IADEMF4 is also found to be more accurate, more efficient, and has better rate of convergence than the benchmarked fourth-order classical iterative methods, namely, the Jacobi (JAC4), the Gauss-Seidel (GS4), and the successive over-relaxation (SOR4) methods.
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13

Doser, D. I. "A Reevaluation of the 1958 Fairweather, Alaska, Earthquake Sequence." Bulletin of the Seismological Society of America 100, no. 4 (July 27, 2010): 1792–99. http://dx.doi.org/10.1785/0120090343.

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14

Lisowski, M., J. C. Savage, and R. O. Burford. "Strain accumulation across the fairweather and Totschunda Faults, Alaska." Journal of Geophysical Research: Solid Earth 92, B11 (October 10, 1987): 11552–60. http://dx.doi.org/10.1029/jb092ib11p11552.

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15

Grouille, Olivier. "BIRD AND FAIRWEATHER IN CONTEXT ASSESSING THE IED THREAT." RUSI Journal 154, no. 4 (August 2009): 40–45. http://dx.doi.org/10.1080/03071840903255252.

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16

Green, Malcolm O., John D. Boon, Jeffrey H. List, and L. Don Wright. "BED RESPONSE TO FAIRWEATHER AND STORM FLOW OH THE SHOREFACE." Coastal Engineering Proceedings 1, no. 21 (January 29, 1988): 112. http://dx.doi.org/10.9753/icce.v21.112.

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Bailard's (1981) model of combined-flow, total-load sediment transport was used to calculate sediment flux at 8-m depth on a wave-dominated shoreface during fairweather and during a storm. Waves were skewed onshore during fairweather, however it was the reversing tidal current that controlled predicted transport direction. Transport direction during the early phase of the storm was also controlled by the mean flow, this time a wind-driven jetlike flow with an offshore component. As the storm progressed, waves became more organized and highly skewed, and by the end of the storm, predicted sediment transport was turned onshore by the shoreward-skewed waves against the mean flow. Measurements of changes in relative bed elevation at the 8-m depth site were used to verify the transport predictions. A total of 6 cm of accretion occurred over H.5 days of low-energy flow. It was found that predicted onshore transport was strongly correlated with erosion at the 8-m depth site, and predicted offshore transport was strongly correlated with accretion. Five cm of scour occurred during the initial phase of the storm, followed by 15 cm of rapid accretion. Onset of accretion was coincident with the organization of surface waves into long-period swell, and the maximum accretion rate was coincident with the most highly-skewed waves.
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17

Bufe, C. G. "Stress Distribution along the Fairweather-Queen Charlotte Transform Fault System." Bulletin of the Seismological Society of America 95, no. 5 (October 1, 2005): 2001–8. http://dx.doi.org/10.1785/0120040171.

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18

Sylvan, Kurt. "Naturalizing Epistemic Virtue Edited By Abrol Fairweather and Owen Flanagan." Analysis 77, no. 3 (June 29, 2017): 663–67. http://dx.doi.org/10.1093/analys/anx076.

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19

Haertl, Kristine. "Factors Influencing Success in a Fairweather Model Mental Health Program." Psychiatric Rehabilitation Journal 28, no. 4 (2005): 370–77. http://dx.doi.org/10.2975/28.2005.370.377.

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20

Boult, Cameron. "Naturalizing Epistemic Virtue, edited by A. Fairweather & O. Flanagan." Journal of Moral Philosophy 14, no. 5 (November 6, 2017): 604–7. http://dx.doi.org/10.1163/17455243-01405004.

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21

McMichael, Philip. "The Relations between Capital and Landed Property: A Reply to Fairweather." Australian and New Zealand Journal of Sociology 23, no. 3 (December 1987): 423–32. http://dx.doi.org/10.1177/144078338702300307.

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22

Lease, Richard O., Peter J. Haeussler, Robert C. Witter, Daniel F. Stockli, Adrian M. Bender, Harvey M. Kelsey, and Paul B. O’Sullivan. "Extreme Quaternary plate boundary exhumation and strike slip localized along the southern Fairweather fault, Alaska, USA." Geology 49, no. 5 (February 22, 2021): 602–6. http://dx.doi.org/10.1130/g48464.1.

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Abstract The Fairweather fault (southeastern Alaska, USA) is Earth’s fastest-slipping intracontinental strike-slip fault, but its long-term role in localizing Yakutat–(Pacific–)North America plate motion is poorly constrained. This plate boundary fault transitions northward from pure strike slip to transpression where it comes onshore and undergoes a <25°, 30-km-long restraining double bend. To the east, apatite (U-Th)/He (AHe) ages indicate that North America exhumation rates increase stepwise from ∼0.7 to 1.7 km/m.y. across the bend. In contrast, to the west, AHe age-depth data indicate that extremely rapid 5–10 km/m.y. Yakutat exhumation rates are localized within the bend. Further northwest, Yakutat AHe and zircon (U-Th)/He (ZHe) ages gradually increase from 0.3 to 2.6 Ma over 150 km and depict an interval of extremely rapid >6–8 km/m.y. exhumation rates that increases in age away from the bend. We interpret this migration of rapid, transient exhumation to reflect prolonged advection of the Cenozoic–Cretaceous sedimentary cover of the eastern Yakutat microplate through a stationary restraining bend along the edge of the North America plate. Yakutat cooling ages imply a long-term strike-slip rate (54 ± 6 km/m.y.) that mimics the millennial (53 ± 5 m/k.y.) and decadal (46 mm/yr) rates. Fairweather fault slip can account for all Pacific–North America relative plate motion throughout Quaternary time and indicates stability of highly localized plate boundary strike slip on a single fault where extreme rock uplift rates are persistently localized within a restraining bend.
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23

Getsos, K., F. Pomoni-Papaioannou, and A. Zelilidis. "A CARBONATE RAMP EVOLUTION IN THE TRANSITION FROM THE APULIA PLATFORM TO THE IONIAN BASIN DURING EARLY TO LATE CRETACEOUS (NW GREECE)." Bulletin of the Geological Society of Greece 40, no. 1 (June 8, 2018): 53. http://dx.doi.org/10.12681/bgsg.16335.

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Facies analysis of Cretaceous carbonate sequences from the external and central Ionian zone revealed a homoclinal ramp model of evolution. During Berriasian to Valanginian, the carbonate ramp was differentiated to an inner-mid and outer ramp environment, which corresponded to the external and central Ionian zone, respectively, while the main inner ramp environment is assumed that was located in the Pre-Apulian zone. The external Ionian zone (inner-mid ramp) is characterized by muds tones-wackes tones with fragmented echinoderms, bivalves, radiolarians and rare aptychus considered to be deposited below the fairweather wave base (FWWB). Locally, thin graded storm deposits intervene, indicating deposition above the storm weather wave base (SWB). Minor occurrences of packs tonesgrainstones, with fragmented echinoderms, calcareous algae, tubiphytes, lagenid foraminifera and rare ooids occur, as well, considered to be deposited at the lowermost part of the inner ramp, near the constantly agitated fairweather wave base (FWWB). The central Ionian zone (outer ramp) is mainly characterized by mudstones-wackestones with abundant radiolarians and rare calpionellids and calcispheres, considered to be deposited below the storm wave base (SWB). No talus or breccias deposits were observed, during the mentioned time interval, in any part of the studied area. From Hauterivian to Turonian, continual sea-level rise, led to establishment of outer ramp environment in the external Ionian zone, over the previous inner-mid ramp, and outer ramp-basin environment, over the previous outer ramp, in the central Ionian zone. The transition from shallower to deeper conditions is characterized by an overall deposition of mudstones-wackestones with abundant radiolarians rooted in pure micrite.
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24

Thenhaus, Paul C., Joseph I. Ziony, William H. Diment, Margaret G. Hopper, David M. Perkins, Stanley L. Hanson, and S. T. Algermissen. "Probabilistic Estimates of Maximum Seismic Horizontal Ground Acceleration on Rock in Alaska and the Adjacent Continental Shelf." Earthquake Spectra 1, no. 2 (February 1985): 285–306. http://dx.doi.org/10.1193/1.1585266.

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Estimates of ground motion hazard from earthquakes in Alaska and the adjacent continental shelf indicate that, for all the exposure times considered, the predicted values of peak acceleration are highest in the Gulf of Alaska and near the major active strike-slip faults of southern Alaska. The evaluations assume a Poisson model of earthquake occurrence and are based on seismic source zones delineated from regional geologic considerations and the historical record of earthquakes. Calculated peak acceleration values for a return period of 100 years range as high as 0.4 g in the Gulf of Alaska sector between Kodiak and Kayak Islands, are about 0.2 g near Anchorage, and 0.1 g near Fairbanks. Values for most of the rest of the state are estimated to be less than .04 g; however, most of the southern Alaska industrial and population base lies within the 0.2 g contour. For a return period of 500 years, peak accelerations are estimated as high as 0.8 g for parts of southeastern Alaska near the Fairweather fault, 0.6 g or greater for part of the Gulf of Alaska, and are about 0.45 g and 0.2 g, respectively, for the Anchorage and Fairbanks areas. Values of acceleration for a return period of 2,500 years exceed 0.6 g for much of southern Alaska and are 0.8 g or greater near the Fairweather and central Denali faults; estimated values are 0.1 g or greater for nearly all of onshore Alaska and for the continental shelf areas of the Bering Sea, Norton and Kotzebue Sounds, southern Chukchi Sea and southeastern Beaufort Sea.
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25

Carter, Anne, Gillian Osmond, and Bronwyn Ormsby. "Ian Fairweather and water-based emulsion house paints in Australia 1950–64." AICCM Bulletin 34, no. 1 (December 2013): 34–43. http://dx.doi.org/10.1179/bac.2013.34.1.005.

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26

Carter, Anne, Gillian Osmond, and Bronwyn Ormsby. "Ian Fairweather and water-based emulsion house paints in Australia 1950–64." AICCM Bulletin 34, no. 1 (December 2014): 34–43. http://dx.doi.org/10.1179/bac.2014.34.1.005.

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27

McAleer, Ryan J., James A. Spotila, Eva Enkelmann, and Aaron L. Berger. "Exhumation along the Fairweather fault, southeastern Alaska, based on low-temperature thermochronometry." Tectonics 28, no. 1 (February 2009): n/a. http://dx.doi.org/10.1029/2007tc002240.

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28

Gottwald, Stephanie, and Margaret Thomas. "Approaches to second language acquisition Ed. by Kari Sajavaara and Courtney Fairweather." Language 74, no. 2 (1998): 429–30. http://dx.doi.org/10.1353/lan.1998.0220.

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29

Fox, Jesse, Michael Gilbert, and Wai Yen Tang. "Player experiences in a massively multiplayer online game: A diary study of performance, motivation, and social interaction." New Media & Society 20, no. 11 (April 11, 2018): 4056–73. http://dx.doi.org/10.1177/1461444818767102.

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Video game researchers have struggled to capture players’ personal experiences in natural gaming contexts. We used longitudinal diary methods to examine the everyday experiences of new and experienced players within a massively multiplayer online game, Team Fortress 2. Participants ( N = 38) completed diaries about gameplay and negative social interactions such as trash-talking and harassment. Themes included frustrating play and performance as motivator, as well as six themes regarding social interaction: skill disparagement, fairweather friends, toxic masculinity, vicious cycles, “kicking” players, and reporting differences. Some findings supported existing research; others challenge previous research using other methods. We discuss the advantages and disadvantages of using diary methods in video game research.
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30

Mandaville, Alison. "Amanat: Women’s Writing from Kazakhstan ed. by Zaure Batayeva and Shelley Fairweather-Vega." World Literature Today 96, no. 5 (September 2022): 56. http://dx.doi.org/10.1353/wlt.2022.0218.

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31

Seidman, Edward. "Fairweather and ESID: Contemporary Impact and a Legacy for the Twenty-First Century." American Journal of Community Psychology 32, no. 3-4 (December 2003): 371–75. http://dx.doi.org/10.1023/b:ajcp.0000004755.51641.d3.

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32

Burton, Robert. "CAPTAIN JAMES FAIRWEATHER: WHALER AND SHIPMASTER: HIS LIFE AND CAREER 1853–1933. Nancy Rycroft. 2005. Ripponden, West Yorkshire: Fairweather Books. 202 p, illustrated, soft cover. ISBN 0-9551739-0-6. £13.95." Polar Record 42, no. 4 (October 2006): 380. http://dx.doi.org/10.1017/s0032247406295755.

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33

Ford, Andrew L. J., Richard R. Forster, and Ronald L. Bruhn. "Ice surface velocity patterns on Seward Glacier, Alaska/Yukon, and their implications for regional tectonics in the Saint Elias Mountains." Annals of Glaciology 36 (2003): 21–28. http://dx.doi.org/10.3189/172756403781816086.

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AbstractSeward Glacier, on the Alaskan/Yukon border along the Gulf of Alaska, sits atop an important structural and morphological junction in the Saint Elias orogen. It is situated at the intersection between the Fairweather and Bagley strike–slip faults, and in the hanging wall of the Malaspina and Chugach–Saint Elias thrust faults. An ice surface velocity map of Seward Glacier derived from interferometric synthetic aperture (InSAR) reveals a complex flow pattern, which implies there is a previously unmapped northwest-trending supra-/subsurface ridge crossing the Seward. Analysis of additional remote-sensing images, ASTER, ERS SAR and the InSAR coherence map, confirms this observation. The presence of this ridge leads to a set of tectonic models describing the possible interaction of the underlying faults.
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34

HAERTL, KRISTINE L. "The Fairweather Mental Health Housing Model—A Peer Supportive Environment: Implications for Psychiatric Rehabilitation." American Journal of Psychiatric Rehabilitation 10, no. 3 (August 28, 2007): 149–62. http://dx.doi.org/10.1080/15487760701508201.

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35

Panneerselvam, C., C. Selvaraj, K. Jeeva, K. U. Nair, C. P. Anilkumar, and S. Gurubaran. "Fairweather atmospheric electricity at Antarctica during local summer as observed from Indian station, Maitri." Journal of Earth System Science 116, no. 3 (June 2007): 179–86. http://dx.doi.org/10.1007/s12040-007-0018-2.

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36

Nabożny, Marcin. "Recenzja: Jack Fairweather, “The Volunteer: One Man, an Underground Army, and the Secret Mission to Destroy Auschwitz”, Harpercollins ­Publishers, New York 2019, pp. 505, ISBN 978-0-06-256141-1." Resovia Sacra 28 (December 31, 2021): 881–85. http://dx.doi.org/10.52097/rs.2021.881-885.

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One man, an underground army, and the secret dogged mission to destroy Auschwitz tells the story of a Polish resistance fighter’s deliberate infiltration of Auschwitz to sabotage the camp from inside, and his struggles up until his death. He defied the odds of suppression as he attempted to warn the Allies about the Nazi’s plan for a “final solution” before it was too late.Jack Fairweather is a British journalist and author. He was born in wales and schooled in Oxford University. He was a war correspondent for British troops during the 2003 invasion of Iraq. In one of those days, as Jack and his friend Matt Mc Allester struggled to makes sense of what they had witness in the wars and putting it in a proper report, Jack came to hear about Witold Pilecki for the first time. He got intrigued as to why someone would risk everything to help his fellow man. He was equally struck by how little was known about Witold’s mission to warn the Western Allies of the Nazi’s crimes. Following Jack’s writing on The Volunteer, he was nominated for Costa Book Award 2019 and shortlisted for biography Award. The book “The Volunteer” is both a historical and biological book that was written by Jack Fairweather and published by HarperCollins Publishers, New York in 2019. It tells the history of the holocaust and gives an account of the untold sacrifice how Witold Pilecki, an average man with no great record of military service, staked his life to reveal Nazi’s greatest crimes when others would rather choose to hide. The book is somewhat provocative, suggesting the tragic defeat of Pilecki’s mission had been caused not in Auschwitz or Berlin, but in London and Washington. The book consists of four parts. Includes acknowledgments, short biography people mentioned in the book, notes, select bibliography and index. The publication is enriched by sixteen maps and a large number of black and white photos.
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37

Joel, Lucas V., Mary L. Droser, and James G. Gehling. "A New Enigmatic, Tubular Organism from the Ediacara Member, Rawnsley Quartzite, South Australia." Journal of Paleontology 88, no. 2 (March 2014): 253–62. http://dx.doi.org/10.1666/13-058.

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Here we reconstruct a new tubular, serially divided organism with a bilateral morphology from the Ediacaran of South Australia. The organism, Plexus ricei new genus new species, was a broadly curving tube that resided on the Ediacaran seafloor. Plexus ricei individuals range in size from 5 to 80 cm long and 5 to 20 mm wide, and are comprised of two main components: a rigid median tubular structure and a fragile outer tubular wall. Plexus ricei is preserved as an external mold on bed soles, and as a counterpart cast on bed tops in sandstones interpreted to represent deposition between storm and fairweather wave-base. The phylogenetic affinities of P. ricei are uncertain; P. ricei symmetry implies a bilaterian origin, but a lack of defined anterior and posterior ends precludes definitive assignment.
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38

Sharrock, Alison. "Alternae Voces—Again." Classical Quarterly 40, no. 2 (December 1990): 570–71. http://dx.doi.org/10.1017/s000983880004324x.

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There is a persistent tradition of reading Propertius 1.10, according to which the Gallus addressed by the poem is the elegiac poet, and the poem itself is a description, not, or not only, of Gallus and his girl in bed but of Propertius reading Gallus’ love elegy.1 In CQ 39 (1989), 561–2, James O'Hara suggests that the phrase ‘in alternis vocibus’ in Prop. 1.10.10 is a hint at amoebean verse, and as such may refer to the amoebean elegiac experiments by Gallus which Fairweather argues are represented by the Qasr Ibrim papyrus. This may well be right. I suggest, however, that the primary metaphorical meaning of ‘in alternis vocibus’ is ‘in your elegiac verse’. Oblique hints at such a reading can be found in Ross (above n. 1), who describes 9f as ‘an extremely suggestive couplet’, and Hinds, in his discussion of alternus as a programmatic term in Ovid, Fasti 4.484.
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39

McKie, Thomas. "A model for marine shelf storm deposition in the Lower Cambrian Fucoid Beds of northwest Scotland." Geological Magazine 127, no. 1 (January 1990): 45–53. http://dx.doi.org/10.1017/s0016756800014151.

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AbstractThe Lower Cambrian Fucoid Beds of northwest Scotland are a 20 m thick mixed clastic-carbonate sequence of thinly bedded storm beds deposited on the western margin of the Iapetus Ocean. Proximal facies display plane beds, current ripple laminations and wave ripple laminations and were deposited under the influence of combined steady andoscillatory currents. The steady component of flow appears to have expanded in an offshore direction and weakened during the final stages of storm deposition with respect to the oscillatory component, producing less asymmetrical ripples with less evidence of a preferred migration direction. Distal facies are represented by thin ‘graded rhythmites’. The palaeocurrent data suggest a wide spread of sediment transport directions, but with a north to northeasterly mode which may reflect a geostrophic component of flow. Following storms these beds were burrowed and echinoderms colonized the sea floor, although the limited extent of these processes and the presence of abundant collophane suggests that the fairweather Fucoid Beds shelf was generally quiescent and possibly dysaerobic.
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40

Haertl, Kristine. "Utilization-Focused Evaluation: Ten-Year Outcomes of a Fairweather Model Mental Health Program—Implications for Occupational Therapy." American Journal of Occupational Therapy 70, no. 4_Supplement_1 (August 1, 2016): 7011510196p1. http://dx.doi.org/10.5014/ajot.2016.70s1-po2033.

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41

Konieczny, Piotr. "Book Review: The Volunteer: The True Story of the Resistance Hero Who Infiltrated Auschwitz by Jack Fairweather." European History Quarterly 51, no. 3 (July 2021): 414–16. http://dx.doi.org/10.1177/02656914211028812b.

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42

Aderhold, K., and R. E. Abercrombie. "Seismic Rupture on an Oceanic-Continental Plate Boundary: Strike-Slip Earthquakes along the Queen Charlotte-Fairweather Fault." Bulletin of the Seismological Society of America 105, no. 2B (April 14, 2015): 1129–42. http://dx.doi.org/10.1785/0120140227.

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43

Wright, L. D., C. R. Sherwood, and R. W. Sternberg. "Field measurements of fairweather bottom boundary layer processes and sediment suspension on the Louisiana inner continental shelf." Marine Geology 140, no. 3-4 (August 1997): 329–45. http://dx.doi.org/10.1016/s0025-3227(97)00032-7.

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44

Carlson, Paul R., Terry R. Bruns, and George Plafker. "Late Cenozoic offsets on the offshore connection between the Fairweather and Queen Charlotte faults off southeast Alaska." Marine Geology 85, no. 1 (December 1988): 89–97. http://dx.doi.org/10.1016/0025-3227(88)90085-0.

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45

Schartman, Anna, Eva Enkelmann, John I. Garver, and Cameron M. Davidson. "Uplift and exhumation of the Russell Fiord and Boundary blocks along the northern Fairweather transform fault, Alaska." Lithosphere 11, no. 2 (January 4, 2019): 232–51. http://dx.doi.org/10.1130/l1011.1.

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46

Baycroft, John. "Pontiflex: A Brief Biographical Note on Some of the Contributions of Canon Eugene Fairweather to the Canadian Church." Toronto Journal of Theology 3, no. 1 (March 1987): 130–33. http://dx.doi.org/10.3138/tjt.3.1.130.

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47

Doser, Diane I. "Seismicity of Southwestern Yukon, Canada, and its relation to slip transfer between the Fairweather and Denali fault systems." Tectonophysics 611 (January 2014): 121–29. http://dx.doi.org/10.1016/j.tecto.2013.11.018.

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48

Kelly, James G., and George W. Fairweather. "The 1985 division 27 award for distinguished contributions to community psychology and community mental health: George W. Fairweather." American Journal of Community Psychology 14, no. 2 (April 1986): 125–37. http://dx.doi.org/10.1007/bf00911816.

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49

Bastow, David. "Religious Education, Ian C. M. Fairweather and J. Norman MacDonald (Scottish Academic Press, 1992), pp. x + 109, £8.50." Scottish Educational Review 25, no. 1 (December 20, 1993): 70–71. http://dx.doi.org/10.1163/27730840-02501012.

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50

Younkin, Eric, and S. Harper Umfress. "Performing a Sonar Acceptance Test of the Kongsberg EM712 Using Open-Source Software: A Case Study of Kluster." Geomatics 2, no. 4 (November 29, 2022): 540–53. http://dx.doi.org/10.3390/geomatics2040029.

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In the world of seafloor mapping, the ability to explore and experiment with a dataset in its raw and processed forms is critical. Kluster is an open-source multibeam data processing software package written in Python that enables this exploration. Kluster provides a suite of multibeam processing features, including analysis, visualization, gridding, and data cleaning. We demonstrated these features using a recently acquired dataset from a Kongsberg EM712 multibeam echosounder aboard NOAA Ship Fairweather. This test dataset served to illustrate the fundamental analysis abilities of the software, as well as its utility as a troubleshooting tool both in the field and during post-processing. Kluster has the capability to perform the Sonar Acceptance Test in full, including common experiments like the patch test, extinction test, and accuracy test, which are generally performed on new systems. When questions arise regarding the integration or parameter settings of a system, this software allows the user to quickly and clearly visualize much of the raw data and its associated metadata, which is a vital step in any investigative effort. With its emphasis on accessibility and ease of use, Kluster is an excellent tool for users who are inexperienced with multibeam sonar data processing.
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