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    The effects of ocean eddies on tropical cyclones

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    Miltenberger_Thesis (9.289Mb)
    Date
    2012-09
    Author
    Miltenberger, Alexander R.  Concept link
    Metadata
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    Citable URI
    https://hdl.handle.net/1912/5354
    Location
    Western Pacific Ocean
    DOI
    10.1575/1912/5354
    Keyword
     Ocean-atmosphere interaction; Oceanic mixing; Roger Revelle (Ship) Cruise RR0912 
    Abstract
    The purpose of this study is to understand the interactions of tropical cyclones with ocean eddies. In particular we examine the influence of a cold-core eddy on the cold wake formed during the passage of Typhoon Fanapi (2010). The three-dimensional version of the numerical Price–Weller–Pinkel (PWP) vertical mixing model has previously been used to simulate and study the cold wakes of Atlantic hurricanes. The model has not been used in comparison with observations of typhoons in the Western Pacific Ocean. In 2010 several typhoons were studied during the Impact of Typhoons on the Ocean in the Pacific (ITOP) field campaign and Fanapi was particularly well observed. We use these observations and the 3DPWP to understand the ocean cold wake generated by Fanapi. The cold wake of Fanapi was advected by a cyclonic eddy that was south of the typhoon track. The 3DPWP model outputs with and without an eddy are compared with observations made during the field campaign. These observations are compared to model outputs with eddies in a series of positions right and left of the storm track in order to study effects of mesoscale eddies on ocean vertical mixing in the cold wake of typhoons.
    Description
    Submitted in partial fulfillment of the requirements for the degree of Master of Science at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution September 2012
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    • Physical Oceanography (PO)
    • WHOI Theses
    Suggested Citation
    Thesis: Miltenberger, Alexander R., "The effects of ocean eddies on tropical cyclones", 2012-09, DOI:10.1575/1912/5354, https://hdl.handle.net/1912/5354
     

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