Relevant bibliographies by topics / Richard M. Weaver

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Academic literature on the topic 'Richard M. Weaver'

Author: Grafiati
Published: 4 June 2021
Last updated: 3 February 2022

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Journal articles on the topic "Richard M. Weaver"

1

Payne, Melinda A., Suzanne M. Ratchford, and Lillian N. Wooley. "Richard M. Weaver: A bibliographical essay." Rhetoric Society Quarterly 19, no. 4 (September 1989): 327–32. http://dx.doi.org/10.1080/02773948909390859.

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Clayton, Bruce, and Fred Douglas Young. "Richard M. Weaver, 1910-1963: A Life of the Mind." Journal of Southern History 63, no. 2 (May 1997): 434. http://dx.doi.org/10.2307/2211335.

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3

Bliese, John R. E. "The conservative rhetoric of Richard M. Weaver: Theory and practice." Southern Communication Journal 54, no. 4 (November 1989): 401–21. http://dx.doi.org/10.1080/10417948909372770.

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Ehrman, John, and Fred Douglas Young. "Richard M. Weaver, 1910-1963: A Life of the Mind." Journal of American History 83, no. 4 (March 1997): 1487. http://dx.doi.org/10.2307/2953047.

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Bliese, John. "Richard M. Weaver and the rhetoric of a lost cause." Rhetoric Society Quarterly 19, no. 4 (September 1989): 313–25. http://dx.doi.org/10.1080/02773948909390858.

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Jacobi, Martin J., and Bernard K. Duffy. "A comprehensive bibliography of works by and about Richard M. Weaver." Rhetoric Society Quarterly 25, no. 1-4 (January 1995): 258–73. http://dx.doi.org/10.1080/02773949509391052.

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Beale, Walter H. "Richard M. Weaver: Philosophical Rhetoric, Cultural Criticism, and the First Rhetorical Awakening." College English 52, no. 6 (October 1990): 626. http://dx.doi.org/10.2307/378029.

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Johannesen, Richard L. "Richard M. Weaver's uses of Kenneth Burke." Southern Speech Communication Journal 52, no. 3 (September 1987): 312–30. http://dx.doi.org/10.1080/10417948709372696.

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Johannesen, Richard L. "A reconsideration of Richard M. Weaver's platonic idealism." Rhetoric Society Quarterly 21, no. 2 (March 1991): 1–10. http://dx.doi.org/10.1080/02773949109390912.

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Zeitlin, Robert N. "Ancient Mesoamerica. A Comparison of Change in Three Regions. Richard E. Blanton, Stephen A. Kowalewski, Gary M. Feinman, and Laura M. Finsten. 2nd edition. Cambridge University Press, Cambridge, 1993. xii + 284 pp., illustrations, tables, references, author index, subject index. $69.95 (paper). - The Aztecs, Maya, and Their Predecessors: Archaeology of Mesoamerica. Muriel Porter Weaver. 3rd edition. Academic Press, San Diego, 1993. xix + 567 pp., illustrations, glossary, references, author index, subject index. $54.95 (cloth)." American Antiquity 60, no. 2 (April 1995): 385–88. http://dx.doi.org/10.2307/282156.

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Books on the topic "Richard M. Weaver"

1

Weaver, Richard M. The southern essays of Richard M. Weaver. Indianapolis: Liberty Press, 1987.

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Young, Fred Douglas. Richard M. Weaver, 1910-1963: A life of the mind. Columbia: University of Missouri Press, 1995.

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3

1949-, Jacobi Martin James, ed. The politics of rhetoric: Richard M. Weaver and the conservative tradition. Westport, Conn: Greenwood Press, 1993.

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Barbarians in the saddle: An intellectual biography of Richard M. Weaver. New Brunswick, NJ: Transaction Publishers, 1997.

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J, Smith Ted, ed. In defense of tradition: Collected shorter writings of Richard M. Weaver, 1929-1963. Indianapolis: Liberty Fund, 2000.

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Scotchie, Joseph A. Barbarians in the Saddle: Intellectual Biography of Richard M. Weaver. Taylor & Francis Group, 2020.

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Scotchie, Joseph A. Barbarians in the Saddle: Intellectual Biography of Richard M. Weaver. Taylor & Francis Group, 2020.

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Scotchie, Joseph A. Barbarians in the Saddle: Intellectual Biography of Richard M. Weaver. Taylor & Francis Group, 2020.

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Scotchie, Joseph A. Barbarians in the Saddle: Intellectual Biography of Richard M. Weaver. Taylor & Francis Group, 2020.

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10

Language is Sermonic: Richard M. Weaver on the Nature of Rhetoric. Louisiana State University Press, 1985.

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Book chapters on the topic "Richard M. Weaver"

1

Ancil, Ralph T. "Richard M. Weaver and the Metaphysics of Property." In The Vision of Richard Weaver, 61–76. Routledge, 2018. http://dx.doi.org/10.4324/9781351293280-3.

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Johannesen, Richard L., Rennard Strickland, and Ralph T. Eubanks. "Richard M. Weaver on the Nature of Rhetoric: An Interpretation." In The Vision of Richard Weaver, 91–100. Routledge, 2018. http://dx.doi.org/10.4324/9781351293280-6.

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Scotchie, Joseph. "The Nation’s Stepchild: The Southern Essays of Richard M. Weaver." In Barbarians in the Saddle, 97–119. Routledge, 2020. http://dx.doi.org/10.4324/9780429336096-7.

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Conference papers on the topic "Richard M. Weaver"

1

Ostrovskii, Alexander, Alexander Ostrovskii, Vyacheslav Lobanov, Vyacheslav Lobanov, Aleksandr Sergeev, Aleksandr Sergeev, Jae-Hun Park, Jae-Hun Park, Young-Gyu Park, and Young-Gyu Park. "MOORED PROFILER OBSERVATIONS OF SUBMESOSCALE COLD-CORE EDDIES IN PETER THE GREAT BAY OF THE EAST/JAPAN SEA IN LATE WINTER." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b4316525691.

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Abstract:
Submesoscale cold-core (T < 0°C) eddies were observed near the shelf break in Peter the Great Bay of the East/Japan Sea in March 2010. The observations were carried out at the moored automatic mobile profiler Aqualog station. The profiling was as frequent as every hour allowing us to obtain data with high temporal resolution. Aqualog delivered vertical profiles of ocean current velocity, acoustic backscatter at 2 MHz, temperature, and salinity between the depths of 20 m and 105 m. Below the profiling range, the InterOcean S4 current meter with temperature and salinity sensors was mounted on the mooring line. Above the profiling range, the RBR XR420 CTD logger with dissolved oxygen, chlorophyll-a fluorescence, and turbidity sensors was also mounted on the mooring line. Additionally we used the data of ship-born CTD casts, the satellite-born imagery and scatterometery, and the coastal weather station records. The data analysis suggests that the cold-core submesoscale eddies play an important role in supplying the densest water (σθ > 27.24 kg/m3) from the northern part of Peter the Great Bay to the shelf break zone where it cascades downward into the deep northern basin of the Sea. The volume of the densest water in an eddy, according to our rough estimate, is 0.5-1 km³. At the sea shelf, the densest water is richer in oxygen by 0.4 ml/l than surrounding water. It also contains much more suspended particles brought by the rivers.
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Ostrovskii, Alexander, Alexander Ostrovskii, Vyacheslav Lobanov, Vyacheslav Lobanov, Aleksandr Sergeev, Aleksandr Sergeev, Jae-Hun Park, Jae-Hun Park, Young-Gyu Park, and Young-Gyu Park. "MOORED PROFILER OBSERVATIONS OF SUBMESOSCALE COLD-CORE EDDIES IN PETER THE GREAT BAY OF THE EAST/JAPAN SEA IN LATE WINTER." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b937b64aa12.88436521.

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Abstract:
Submesoscale cold-core (T < 0°C) eddies were observed near the shelf break in Peter the Great Bay of the East/Japan Sea in March 2010. The observations were carried out at the moored automatic mobile profiler Aqualog station. The profiling was as frequent as every hour allowing us to obtain data with high temporal resolution. Aqualog delivered vertical profiles of ocean current velocity, acoustic backscatter at 2 MHz, temperature, and salinity between the depths of 20 m and 105 m. Below the profiling range, the InterOcean S4 current meter with temperature and salinity sensors was mounted on the mooring line. Above the profiling range, the RBR XR420 CTD logger with dissolved oxygen, chlorophyll-a fluorescence, and turbidity sensors was also mounted on the mooring line. Additionally we used the data of ship-born CTD casts, the satellite-born imagery and scatterometery, and the coastal weather station records. The data analysis suggests that the cold-core submesoscale eddies play an important role in supplying the densest water (σθ > 27.24 kg/m3) from the northern part of Peter the Great Bay to the shelf break zone where it cascades downward into the deep northern basin of the Sea. The volume of the densest water in an eddy, according to our rough estimate, is 0.5-1 km³. At the sea shelf, the densest water is richer in oxygen by 0.4 ml/l than surrounding water. It also contains much more suspended particles brought by the rivers.
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