Journal ArticleThe Structural Compactness of a Tropical Cyclone Seed Affects Its PersistenceLu, Kuan-Yu; Chavas, Daniel R; Wang, Danyang<title>Abstract</title> <p>Tropical cyclones (TCs) are often generated from preexisting “seed” vortices. Seeds with higher persistence might have a higher chance to undergo TC genesis. What controls seed persistence remains unclear. This study proposes that planetary Rossby wave drag is a key factor that affects seed persistence. Using recently developed theory for the response of a vortex to the planetary vorticity gradient, a new parameter given by the ratio of the maximum wind speed (<italic>V</italic>_max) to the Rhines speed at the radius of maximum wind (<italic>R</italic>_max), here termed “vortex structural compactness” (<italic>C_υ</italic>), is introduced to characterize the vortex weakening by planetary Rossby wave drag. The relationship between vortex compactness and weakening rate is tested via barotropic<italic>β</italic>-plane experiments. The vortex’s initial<italic>C_υ</italic>is varied by systematically varying their initial<italic>V</italic>_maxand<italic>R</italic>_maxin idealized wind profile models. Experiments are also conducted with real-world seed vortices from reanalysis data, which possess natural compactness variability. The weakening rate depends strongly on the vortex’s initial<italic>C_υ</italic>across both idealized and real-world experiments, and the initial axis-asymmetry introduces minor differences. Experiments doubling the size of seed vortices cause them to weaken more rapidly, in line with other experiment sets. The dependence of the weakening rate on initial compactness can be predicted from a simple theory, which is more robust for more compact vortices. Our results suggest that a seed’s structure strongly modulates how long it can persist in the presence of a planetary vorticity gradient. Connections to real seeds on Earth are discussed.</p> <sec><title>Significance Statement</title><p>This study explores the evolution of tropical cyclone (TC) seeds, which are preexisting weakly rotating rainstorms, in a simple setting that isolates the dynamical effects of the rotating sphere. It is not clear why some seeds can persist for a longer duration and might have a higher chance to eventually undergo genesis. We proposed that a factor called “planetary Rossby wave drag” plays a crucial role in this process. To investigate this, we introduce a new parameter called “compactness” to describe how the size and intensity of a seed vortex determines how quickly it will weaken due to this drag. We conducted experiments with numerical simulations and real-world TC seeds to test our ideas. Our findings show that the initial compactness of seeds strongly influences how quickly they weaken. We have developed a formula to predict how quickly these seeds weaken based on their compactness, which is especially accurate for more compact seeds. This research helps us understand how planetary Rossby wave drag affects the persistence of a TC seed and, ultimately, how it might impact the frequency of TCs.</p></sec>American Meteorological Society2025-05-0110593537Journal of the Atmospheric Sciences825999 to 10140022-4928https://doi.org/10.1175/JAS-D-23-0149.11945113; 2431970National Science Foundation