Authors: Sherry Young*, George Mason University, Barry A Klinger, George Mason University, Randolph A McBride, George Mason University
Topics: Climatology and Meteorology, Hazards, Risks, and Disasters, Oceanography
Keywords: Loop Current, Gulf of Mexico, hurricanes, Katrina, rapid intensification, ocean heat content, climate change, oceanography, tropical cyclones, storms, ocean currents
Session Type: Poster
Start / End Time: 8:00 AM / 9:40 AM
Room: Lincoln 2, Marriott, Exhibition Level
Presentation File: Download
Increasing population in coastal communities is putting more lives and property at risk from hurricanes. A great need exists for a better understanding of hurricane intensity and rapid intensification; especially if intensity could increase because of warming oceans. Eleven Gulf of Mexico hurricanes and their fluctuations in intensity relative to proximity to the Loop Current, ocean heat content, depth to the 26°C isotherm, and SST were investigated. ESRI ArcMap was utilized to map and relate hurricane and ocean surface layer data obtained by satellite, reanalysis products, and NHC data. 164 data points were binned to sort by proximity to the Loop Current and to isolate other factors such as eyewall replacement cycles and wind shear. Linear regression was used to calculate correlations between variables and intensity, percent of maximum potential intensity (MPI), and to calculate probability of rapid intensification. Katrina had the best correlation between sustained wind speed and ocean heat content at 91% during rapid intensification episodes. During favorable conditions, data points with the highest sustained wind speeds of 250 km/hr or more and reached 100% of MPI occurred where SST was 29.75°C or greater, depth to the 26°C isotherm was 50 m or more, and TCHP was 90 kJ/cm² or more. During favorable conditions hurricanes were more likely to rapidly intensify 57.1% over the LC than GCW at 40%. Results suggest that increased ocean heat content and depth to the 26°C isotherm in the Loop Current limits surface cooling due to mixing permitting additional intensification during favorable conditions.