Relevant bibliographies by topics / Hurricane Frederick

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Academic literature on the topic 'Hurricane Frederick'

Author: Grafiati
Published: 4 June 2021
Last updated: 29 July 2025

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Journal articles on the topic "Hurricane Frederick"

1

Schneider, R. W., C. A. Hollier, H. K. Whitam, et al. "First Report of Soybean Rust Caused by Phakopsora pachyrhizi in the Continental United States." Plant Disease 89, no. 7 (2005): 774. http://dx.doi.org/10.1094/pd-89-0774a.

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Asian soybean rust, caused by Phakopsora pachyrhizi Sydow, has been known to occur in the eastern hemisphere for nearly a century. More recently, it was reported from Hawaii in 1994, eastern and southern Africa from 1996-1998, Nigeria in 2001, and Brazil and Paraguay in 2002. Aerobiological models suggested that urediniospores of the pathogen would be disseminated on wind currents to the continental United States in association with tropical storms if the disease became established north of the equator during hurricane season (U.S. Soybean Rust Detection and Aerobiological Modeling online publ
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2

Krishnamurthi, T. N., H. S. Bedi, Darlene Oosterhof, and Vivek Hardiker. "The Formation of Hurricane Frederic of 1979." Monthly Weather Review 122, no. 6 (1994): 1050–74. http://dx.doi.org/10.1175/1520-0493(1994)122<1050:tfohfo>2.0.co;2.

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3

Shay, Lynn K., and Russell L. Elsberry. "Near-Inertial Ocean Current Response to Hurricane Frederic." Journal of Physical Oceanography 17, no. 8 (1987): 1249–69. http://dx.doi.org/10.1175/1520-0485(1987)017<1249:niocrt>2.0.co;2.

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4

Kaplan, John, and William M. Frank. "The Large-Scale Inflow-Layer Structure of Hurricane Frederic (1979)." Monthly Weather Review 121, no. 1 (1993): 3–20. http://dx.doi.org/10.1175/1520-0493(1993)121<0003:tlsils>2.0.co;2.

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5

Ksit, Barbara, and Anna Szymczak-Graczyk. "Rare Weather Phenomena and the Work of Large-Format Roof Coverings." Civil and Environmental Engineering Reports 29, no. 3 (2019): 123–33. http://dx.doi.org/10.2478/ceer-2019-0029.

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Abstract Wind action belongs to loads that are environmentally variable. Wind action is included in the basic combination of loads, whereas hurricane wind action is classified as a unique combination. Due to large gusts of wind, the roof coverings of large-scale buildings are exposed to detachment of their cover layer. The article presents the effects of over-normative wind, which occurred on January 19, 2018 and was named the cyclone Frederic/David. The purpose of the article is to show that in design of roof coverings made of large-format materials, such as membranes, it is crucial to accept
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6

Conte, J. P., and P. W. Marshall. "Low-Frequency Forces on Tubular Spaceframe Towers: Analysis of Cognac Data." Journal of Offshore Mechanics and Arctic Engineering 116, no. 3 (1994): 122–26. http://dx.doi.org/10.1115/1.2920140.

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The Cognac field data indicate that the low-frequency force response components are not negligible and are significantly correlated to the wave envelope process. Although this is a well-known phenomenon in floating structures, it had previously not been validated from data recorded on fixed platforms. Simulation studies based on a vertical rigid cylinder subjected to Hurricane Frederic sea states show significant differences in applied low-frequency drag forces obtained using the Wheeler and Delta stretching schemes used to approximate near-surface fluid kinematics. Previous studies focusing o
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7

Nogueira, Ricardo C., and Barry D. Keim. "Annual Volume and Area Variations in Tropical Cyclone Rainfall over the Eastern United States." Journal of Climate 23, no. 16 (2010): 4363–74. http://dx.doi.org/10.1175/2010jcli3443.1.

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Abstract This paper examines tropical cyclone (TC) rainfall in the eastern United States from the perspective of documenting accumulated annual water volumes and areas of the precipitation. Volume is a value that merges both rainfall depth and rainfall area into a single metric for each year that can be directly compared between individual years. Area represents the total land area affected by tropical rains. These TC rainfall metrics were then compared to the ENSO and the Atlantic multidecadal oscillation (AMO). Time series of annual TC water volumes show an annual average of 107 km3. The max
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8

Froede, Carl R. "A Hurricane Frederic–Generated Storm-Surge Deposit Exposed along a Surf-Zone Foredune Scarp on Dauphin Island, Alabama, U.S.A." Journal of Coastal Research 222 (March 2006): 371–76. http://dx.doi.org/10.2112/04-0174.1.

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9

Ngoc Le, Ly. "A numerical study of sea level and current responses to Hurricane Frederic using a coastal ocean model for the Gulf of Mexico." Journal of Oceanography 50, no. 6 (1994): 599–616. http://dx.doi.org/10.1007/bf02270494.

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10

Otvos, Ervin G. "Discussion of: FROEDE, C.R., JR., 2006. A Hurricane Frederic–Generated Storm-Surge Deposit Exposed Along a Surf-Zone Foredune Scarp on Dauphin Island, Alabama, U.S.A.Journal of Coastal Research, 22, 371–376." Journal of Coastal Research 225 (September 2006): 1305. http://dx.doi.org/10.2112/1551-5036(2006)22[1305:dofcja]2.0.co;2.

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Books on the topic "Hurricane Frederick"

1

M, Frank William, and United States. National Aeronautics and Space Administration., eds. Analysis of the inflow and air-sea interactions in hurricane Frederic (1979): Final report. National Aeronautics and Space Administration, 1986.

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2

Haskins, Michael. Car wash blues: A Mick Murphy Key West mystery. Five Star/Gale, 2012.

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Journal articles
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