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Jeffrey P. Donnelly. Woodruff, Jonathan Dalrymple Woods Hole Oceanographic Institution. Joint Program in Oceanography/Applied Ocean Science and Engineering Woods Hole Oceanographic Institution Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences 2010-05-27T19:47:22Z 2010-05-27T19:47:22Z 2009 2009 http://hdl.handle.net/1721.1/55332 430044937 Thesis (Ph. D.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2009. Includes bibliographical references. Tropical cyclone activity over the last 5000 years is investigated using overwash sediments from coastal lagoons on the islands of Vieques, Puerto Rico and Koshikijima, Japan. A simple sediment transport model can reproduce the landward fining deposits observed at Vieques, and reveals that although the record exhibits centennial-tomillennial changes in hurricane overwash frequency, the magnitude of these flooding events has remained relatively constant. Stochastic simulations of hurricane overwash show that breaks in activity at Vieques are extremely long and unlikely to occur under the current hurricane climatology and the present barrier morphology. Periods of less frequent hurricane deposition at Vieques are contemporaneous with intervals of increased El Nifio occurrences and reduced precipitation in West Africa, suggesting a dominant influence by these two climatic phenomena. Hiatuses in overwash activity between 3600-to-2500 and 1000-500 years ago are longer than what is generated by overwash simulations under a constant El Niflo-like state, indicating that mechanisms in addition to variability in the El Nifio/Southern Oscillation are required to completely produce the overwash variability at Vieques. Periods of low overwash activity at Vieques are concurrent with increased overwash activity at Kamikoshiki and may indicate a correspondence between tropical cyclone activity in the western Northern Atlantic and the western North Pacific. by Jonathan D. Woodruff. Ph.D. 106 leaves eng Massachusetts Institute of Technology M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. http://dspace.mit.edu/handle/1721.1/7582 Earth, Atmospheric, and Planetary Sciences. /Woods Hole Oceanographic Institution. Joint Program in Oceanography/Applied Ocean Science and Engineering. Woods Hole Oceanographic Institution. Tropical cyclones within the sedimentary record : analyzing overwash deposition from event to millennial timescales Thesis application/pdf Publication unknown unknown <Publication xmlns="https://www.openaire.eu/cerif-profile/1.1/" id="aae4876b-23ee-4fe0-8919-995da49b838e"> <Type xmlns="https://www.openaire.eu/cerif-profile/vocab/COAR_Publication_Types">http://purl.org/coar/resource_type/c_1843</Type> <Language>eng</Language> <Title>Tropical cyclones within the sedimentary record : analyzing overwash deposition from event to millennial timescales</Title> <PublishedIn> <Publication> </Publication> </PublishedIn> <PublicationDate>2009</PublicationDate> <Authors> <Author> <DisplayName>Woodruff, Jonathan Dalrymple</DisplayName> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> </Authors> <Editors> </Editors> <Publishers> <Publisher> <DisplayName>Massachusetts Institute of Technology</DisplayName> <OrgUnit /> </Publisher> </Publishers> <License>http://dspace.mit.edu/handle/1721.1/7582</License> <Keyword>Earth, Atmospheric, and Planetary Sciences.</Keyword> <Keyword>/Woods Hole Oceanographic Institution. Joint Program in Oceanography/Applied Ocean Science and Engineering.</Keyword> <Keyword>Woods Hole Oceanographic Institution.</Keyword> <Abstract>Tropical cyclone activity over the last 5000 years is investigated using overwash sediments from coastal lagoons on the islands of Vieques, Puerto Rico and Koshikijima, Japan. A simple sediment transport model can reproduce the landward fining deposits observed at Vieques, and reveals that although the record exhibits centennial-tomillennial changes in hurricane overwash frequency, the magnitude of these flooding events has remained relatively constant. Stochastic simulations of hurricane overwash show that breaks in activity at Vieques are extremely long and unlikely to occur under the current hurricane climatology and the present barrier morphology. Periods of less frequent hurricane deposition at Vieques are contemporaneous with intervals of increased El Nifio occurrences and reduced precipitation in West Africa, suggesting a dominant influence by these two climatic phenomena. Hiatuses in overwash activity between 3600-to-2500 and 1000-500 years ago are longer than what is generated by overwash simulations under a constant El Niflo-like state, indicating that mechanisms in addition to variability in the El Nifio/Southern Oscillation are required to completely produce the overwash variability at Vieques. Periods of low overwash activity at Vieques are concurrent with increased overwash activity at Kamikoshiki and may indicate a correspondence between tropical cyclone activity in the western Northern Atlantic and the western North Pacific.</Abstract> <Access xmlns="http://purl.org/coar/access_right" > </Access> </Publication>