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Exploring a Global Climatology of Tropical Cyclone Eye Sizes ETHAN WRIGHT: UNC ASHEVILLE RESEARCH ADVISOR: DR. CHRISTOPHER HENNON 04/22/2015
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Peak Intensity: 190 mph Lowest Pressure: 870 mb Small eye size of 8 nm Super Typhoon Tip (1979)
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Super Typhoon Winnie (1997) Peak Intensity: 160 mph Outer ring of convection: 200 nm
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Goal of this Study Use a consensus of eye sizes to find the correlation of eye sizes to estimated intensities through analysis of tropical cyclone images classified through Cyclone Center.
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Cyclone Center A web site dedicated to the global analysis of archived satellite images of tropical cyclones by “Citizen Scientists”. Images are analyzed through a set of questions related to the Dvorak Technique. User responses are recorded and transferred to a number that can be related to a maximum surface wind speed.
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Power in Numbers Crowd sourcing has proven to be an effective means of addressing large data sets HURSAT data contain nearly 3,000 storms, 300,000 images
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Jordan 1961 Related MSLP to changes in eye diameter. Weatherford and Gray 1988 Weak Correlation between MSLP and outer-core strength alone. A more direct relationship between MSLP and outer-core strength is evident when also accounting for eye size. Kodama and Yamada et al. 2005 Compared IR satellite images to microwave imagery from the Tropical Rainfall Measurement Mission (TRMM) between 1998-2002. Past Research
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Disadvantages TC Eye often obscured by cirrus shield Coarse Resolution of 8 KM Advantages Global Coverage Continuous Data 32 Years of Data Advantages and Disadvantages of Using IR Images
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Users Weighted by: Number of Classifications Completed How well user classified “eye storms”
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Very low statistical correlation between eye size and intensity through estimated Dvorak classification values. Average eye size classification for tropical storms: 46 km Average eye size of tropical cyclones (>64 kts): 34 km Average “eye storm” wind speed classification: 108 kts Results
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Possible Future Work Investigation of TC eye size changes through life cycle stages. Spatial changes with TC Eye sizes.
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References Anthes, R. A., 1982: Tropical Cyclones: Their Evolution, Structure and Effects. Science Press, 208 pp. Candis L. Weatherford and William M. Gray, 1988: Typhoon Structure as Revealed by Aircraft Reconnaissance. Part II: Structural Variability. Mon. Wea. Rev., 116, 1044–1056. C. L. Jordan, 1961: MARKED CHANGES IN THE CHARACTERISTICS OF THE EYE OF INTENSE TYPHOONS BETWEEN THE DEEPENING AND FILLING STAGES. J. Meteor., 18, 779–789. Dvorak, V. F., 1975: Tropical cyclone intensity analysis and forecasting from satellite imagery. Mon. Wea. Rev., 103, 420–430. Hennon, C. C., and Coauthors, 2015: Cyclone Center: Can Citizen Scientists Improve Tropical Cyclone Intensity Records?. Bull. Amer. Meteor. Soc. Yasu-Masa Kodama and Takuya Yamada, 2005: Detectability and Configuration of Tropical Cyclone Eyes over the Western North Pacific in TRMM PR and IR Observations. Mon. Wea. Rev., 133, 2213– 2226.
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