Fortunately for operational forecasting, our findings indicate that probabilities of TC genesis scale well with both lead-time and Dvorak T-number. Pre-genesis disturbances that are analyzed at higher Dvorak intensities are generally found to have a greater likelihood of subsequent genesis into a tropical depression and/or storm. Differences in TC formation definition and potential between basins will be discussed. For example, for a given T-number, systems in the western North Pacific have the greatest likelihood of become a TC. Furthermore, systems in the North Indian Ocean show the longest lead-time before genesis while the Southern Hemisphere basins exhibit the shortest lead-time. Statistics on both pre-genesis and non-genesis systems will be shown, along with comparisons that show the distribution of systems and Dvorak classifications between basins.
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