Development of frontal boundaries during the extratropical transition of tropical cyclones

This study seeks to characterize the development of atmospheric fronts during the extratropical transition (ET) of tropical cyclones (TCs) as a function of their evolution during ET. Composite histograms indicate that the magnitude of the lower atmospheric frontogenesis and average sea-surface temperature is different based on the nature of the TC's structural change during ET. We find that the development of cold and warm fronts evolves as expected from conceptual models of extratropical cyclones. Composites of these fronts relative to the completion of ET show that azimuth, storm motion, and deep-layer shear all appear to have equal influence on the frontal positions. TCs that have more fronts at the time of ET onset complete ET more quickly, suggesting that pre-existing fronts before ET begins may contribute to a shorter ET duration. The orientations of fronts at ET completion in the North Atlantic and west Pacific align with the climatological distributions of the sea-surface temperatures associated with the western boundary currents in each of those basins. These results provide a perspective on the locations of frontal development within TCs undergoing ET. This study characterizes the development of atmospheric fronts during the extratropical transition of tropical cyclones in a reanalysis dataset. The development of cold and warm fronts develops as expected from conceptual models. More fronts present at the beginning of extratropical transition may contribute to a shorter duration of that process. The orientation of fronts at the completion of extratropical transition aligns with climatological distributions of sea surface temperatures in the Atlantic and Pacific.image