20,145 research outputs found
Faculty recital, February 17, 1975 : Thomas Hardie, baritone
No full textRecorded during a live performance at Oakland Recital Hall, Western Michigan University, Kalamazoo, Michigan, February 17, 1975, program no. 162 of the Department of Music's 1974-1975 season.Thomas Hardie, baritone ; accompanist, Steven Hesla, piano and harpsichord. Assisted by: David Kalfsbeek, Peter Delille, Richard Uren, Thomas Shannon, trombones (1st work).Reel 1: Fili mi, Absalon / Heinrich Schütz -- (6:54) Sorrow, sorrow, stay / John Dowland -- (10:27) Floridante. Aria di Floridante [Alma mia?] ; (15:42) Berenice. Si, tra i ceppi / George Frederick Handel -- (25:51) Oh! quand je dors / Franz Liszt -- Chansons gaillardes. (31:03) La maîtresse volage ; (31:53) Chanson à boire ; (34:59) Sérénade / Francis Poulenc -- (38:02) Phydilé [i.e. Phidylé] / Henri Duparc.Reel 2: Ballade in G minor, op. 23 / Frédéric Chopin (Steven Hesla, piano) -- Flight for heaven: a cycle of Robert Herrick songs. (10:28) To Music, to becalm his Fever ; (12:53) Cherry-Ripe ; (14:49) Upon Julia's Clothes; (15:32) To Daisies, not to shut so Soon; (16:13) Epitaph; (17:13) Another Epitaph; (18:05) To the Willow-tree; (20:09) Comfort to a Youth that had lost his Love; (22:26) (Piano Interlude); (23:59) To Anthea, who may command him Anything / Ned Rorem
Impact of coupling an ocean model to WRF nor’easter simulations
No full textThe impact of ocean-atmosphere coupling and its possible seasonal dependence upon Weather Research and Forecasting (WRF) model simulations of seven, winter-time cyclone events was investigated. Model simulations were identical aside from the degree of ocean model coupling (static SSTs, 1D mixed-layer model, full-physics 3D ocean model). Both 1D and 3D ocean model coupling simulations show that SSTs following the passage of a nor’easter did tend to cool more strongly during the early season (Oct-Dec) and were more likely to warm late in the season (Feb-Apr). Model simulations produce SST differences of up to 1.14 K, but this change did not lead to significant change in storm track ( 1) and have low-to-moderate threat scores (0.31 – 0.59). Analysis of the storm environment and the overall simulation failed to reveal any statistically significant differences in model error attributable to ocean-atmosphere coupling. Despite this result, ocean model coupling can reduce dynamical field error at a single level by up to 20%, and this was slightly greater (1-2%) with 3D ocean model coupling as compared to 1D ocean model coupling. Thus, while 3D ocean model coupling tended to generally produce more realistic simulations, its impact would likely be more profound for longer-term simulations.© Copyright 2015 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act September 2010 Page 2 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108, as revised by P.L. 94-553) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a web site or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. Additional details are provided in the AMS Copyright Policy, available on the AMS Web site located at (http://www.ametsoc.org/) or from the AMS at 617-227-2425 or [email protected] reviewe
Impact of Coupling an Ocean Model to WRF Nor’easter Simulations
No full textThe impact of ocean–atmosphere coupling and its possible seasonal dependence upon Weather Research and Forecasting (WRF) Model simulations of seven, wintertime cyclone events was investigated. Model simulations were identical aside from the degree of ocean model coupling (static SSTs, 1D mixed layer model, full-physics 3D ocean model). Both 1D and 3D ocean model coupling simulations show that SSTs following the passage of a nor’easter did tend to cool more strongly during the early season (October–December) and were more likely to warm late in the season (February–April). Model simulations produce SST differences of up to 1.14 K, but this change did not lead to significant changes in storm track ( 1) and have low-to-moderate threat scores (0.31–0.59). Analysis of the storm environment and the overall simulation failed to reveal any statistically significant differences in model error attributable to ocean–atmosphere coupling. Despite this result, ocean model coupling can reduce dynamical field error at a single level by up to 20%, and this was slightly greater (1%–2%) with 3D ocean model coupling as compared to 1D ocean model coupling. Thus, while 3D ocean model coupling tended to generally produce more realistic simulations, its impact would likely be more profound for longer-term simulations.© Copyright 2015 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act September 2010 Page 2 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108, as revised by P.L. 94-553) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a web site or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. Additional details are provided in the AMS Copyright Policy, available on the AMS Web site located at (http://www.ametsoc.org/) or from the AMS at 617-227-2425 or [email protected] reviewe
"The Translingual Sensibility: A Conversation Between Steven G. Kellman and Ilan Stavans"
Get PDFDialogue might be the most appropriate medium for reflections on translingualism. In a dialogue conducted by email over the course of ten days, Steven G. Kellman and Ilan Stavans consider the validity and implications of linguistic determinism. Their conversation examines whether some words that seem to embody the unique Weltanschaaung of a particular culture – such as Schadenfreude, duende, or mångata – can be appropriated, if not translated, into another culture. Pondering whether there are any inherent qualities that distinguish texts by monolingual writers such as Jane Austen and William Faulkner from work by authors who switch languages, such as Samuel Beckett and Vladimir Nabokov, they agree on the usefulness of thinking in terms of a translingual sensibility. Apart from the biographical circumstances of the author, a text possesses a translingual sensibility if it embodies an awareness of both the power and the limitations of its own verbal medium
Kapitalistische Kognition: Steven G. Marks erklärt Informationsgewinnung zum systembildenden Faktor
Get PDFSteven G. Marks: The Information Nexus: Global Capitalism from the Renaissance to the Present. Cambridge: Cambridge University Press 2016. 978-1-107-10868-
A Cross-Layer Multicast-Push Unicast-Pull (MPUP) Architecture for Reliable File-Stream Distribution
No full textThe growing deployment of OpenFlow/SDN networks makes it increasingly possible to leverage network multi-cast services. This work proposes a novel cross-layer Multicast- Push Unicast Pull (MPUP) architecture that includes functionality in the application, transport and link layers to offer users a reliable file-stream distribution service to multiple subscribers. A prototype implementation of the MPUP architecture was realized in a new version of Local Data Manager (LDM), LDM7, a software program that has been in use since 1994 for real-time meteorology data distribution. LDM6, the currently deployed version, uses application-layer multicast. Experiment were run on the GENI infrastructure to compare LDM7 and LDM6. The two main findings are (i) LDM7 can be run at a higher sending rate than LDM6 allowing for improved performance (lower file-delivery latency), and (ii) to achieve the same performance, LDM7 uses significantly lower bandwidth and compute capacity. A three-fold improvement in performance improvement was possible with LDM7, and a bandwidth reduction from 350 Mbps to 21.4 Mbps was observed with 24 receivers.Peer reviewe
Book Review: Vulnerable Subjects: Ethics and Life Writing
No full textAuthor: G. Thomas Couser
Reviewer: Steven Brown
Publisher: (Ithaca: Cornell, 2004).
Cost: Paperback - 47.50
Paper, 2003 ISBN: 0-8014-8863-X 47.50
Sound enhancements for graphical simulations
Get PDFThesis (M.S.)--Massachusetts Institute of Technology, Dept. of Mechanical Engineering, 1997.Includes bibliographical references (p. 117).prepared by Steven G. Villareal.M.S
Fauna associated with the nests of Crocodylus moreletii and Crocodylus moreletii × acutus in Belize
No full textPlatt, Steven G., Rainwater, Thomas R., McMurry, Scott T. (2021): Fauna associated with the nests of Crocodylus moreletii and Crocodylus moreletii × acutus in Belize. Journal of Natural History 55 (3-4): 133-149, DOI: 10.1080/00222933.2021.1895350, URL: http://dx.doi.org/10.1080/00222933.2021.189535
FIGURES 2A–G in Systematics of the New Zealand Weevil Etheophanus Broun (Curculionidae: Molytinae)
No full textFIGURES 2A–G. Lateral habiti of Etheophanus spp. A, E. kuscheli sp. n.; B, E. nitidellus; C, E. optandus; D, E. pingius; E, E. striatus.Published as part of Davis, Steven R., Brav-Cubitt, Talia, Buckley, Thomas R. & Leschen, Richard A. B., 2019, Systematics of the New Zealand Weevil Etheophanus Broun (Curculionidae: Molytinae), pp. 341-374 in Zootaxa 4543 (3) on page 345, DOI: 10.11646/zootaxa.4543.3.2, http://zenodo.org/record/261784
- …
