Daily Tropical Cyclone Intensity Response to Solar Ultraviolet Variations

Astronomy and Astrophysics – Astrophysics

Scientific paper

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[0360] Atmospheric Composition And Structure / Radiation: Transmission And Scattering, [1650] Global Change / Solar Variability, [3305] Atmospheric Processes / Climate Change And Variability, [7536] Solar Physics, Astrophysics, And Astronomy / Solar Activity Cycle

Scientific paper

An inverse relationship between hurricane frequency and intensity over the Caribbean and the number of sunspots has been recently identified. Here we investigate this relationship and find support for the hypothesis that changes in ultraviolet (UV) radiation rather than changes in other concomitant solar and cosmic variations are the cause. The relationship is statistically significant after accounting for variation in ocean heat and the El Niño cycle. A cooling response in the upper troposphere due to decreased solar UV forcing on photochemistry, radiative heating, and dynamics in the stratosphere increases the atmosphere's convective available potential energy leading to a stronger cyclone. The mean amplitude of the intensity response is 4.3 ± 1.86 m/s per 0.01 Mg II units (s.d.), which is quantitatively consistent with the heat-engine theory of tropical cyclone intensity but is less sensitive by a factor of 2 to 3 to an equivalent amount of warming at the ocean surface.

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