Document Type
Dissertation
Degree
Doctor of Philosophy (PhD)
Major/Program
Earth Systems Science
First Advisor's Name
Haiyan Jiang
First Advisor's Committee Title
Committee chair
Second Advisor's Name
Hugh Willoughby
Second Advisor's Committee Title
Committee member
Third Advisor's Name
Ping Zhu
Third Advisor's Committee Title
Committee member
Fourth Advisor's Name
Arturo Leon
Fourth Advisor's Committee Title
Committee member
Keywords
Tropical cyclones, precipitation, rainfall rate, remote sensing
Date of Defense
6-27-2022
Abstract
Estimating the magnitude of tropical cyclone (TC) rainfall at different landfalling states is an important aspect of the TC forecast that directly affects the level of response from emergency managers in coastal areas. This research analyses the spatial distribution of the rainfall magnitude in tropical cyclones (TCs) at different stages over global oceans. The research’s central hypothesis is that TC rainfall exhibits distinct features in the long-term satellite dataset due to the evolution of the spatial distribution, radial variation, and asymmetries at the stages before, during, and after landfall. The resulting patterns are analyzed through a statistical approach that takes advantage of a 20-year global satellite database of rainfall retrievals from the TRMM/GPM constellation, with the aim to achieve two main objectives: 1) The first objective was to explore the global trends of TC rainfall rates using observational evidence provided by a satellite-based climatology. Results indicate there is an increasing trend in the global average TC rainfall rate of about 1.3% per year, with a more pronounced trend in the northern hemisphere than in the southern hemisphere. 2) The second objective was to examine the spatial distribution of the magnitude and axisymmetric intensity profiles of rainfall over the six TC-prone basins. The obtained differences were quantitatively investigated in terms of geographic location, sub-regions within the storm, and TC intensities. Results indicate that major hurricanes in the Atlantic basin exhibit heavier inner-core rainfall rates than those in any other basins, and this difference is highly correlated to specific environmental conditions. Overall, with the achievement of the above-described objectives, this document identifies and summarizes the dominant factors that control rainfall distribution in global TCs, mainly focused on the differences during landfilling processes.
Identifier
FIDC010719
ORCID
https://orcid.org/0000-0001-6076-2347
Previously Published In
Guzman, O., & Jiang, H. (2021). Heavier Inner-Core Rainfall of Major Hurricanes in the North Atlantic Basin Than in Other Global Basins, Journal of Climate, 34(14), 5707-5721.
Guzman, O. and H. Jiang, 2021: Global Increase in Tropical Cyclone Rain Rate. Nature Communications. 12, 5344.
Guzman, O., & Jiang, H. (2022). Climatology of Tropical Cyclone Rainfall Magnitude at Different Landfalling Stages. Journal of Applied Meteorology and Climatology. (In process of publication)
Recommended Citation
Guzman Rey, Oscar, "Climatology of Rainfall Distribution and Asymmetries of Tropical Cyclones: A Global Perspective" (2022). FIU Electronic Theses and Dissertations. 5075.
https://digitalcommons.fiu.edu/etd/5075
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