An Observational Analysis of Tropical Cyclone Recurvature.

1991 ◽  
Author(s):  
Stephen J. Hodanish
1993 ◽  
Vol 121 (10) ◽  
pp. 2665-2689 ◽  
Author(s):  
Stephen Hodanish ◽  
William M. Gray

2017 ◽  
Vol 74 (8) ◽  
pp. 2489-2502 ◽  
Author(s):  
Morgan E O’Neill ◽  
Diamilet Perez-Betancourt ◽  
Allison A. Wing

Abstract A recent observational analysis has reported significant repeating diurnal signals propagating outward at cloud-top height from tropical cyclone centers. Modeling studies suggest that the visible upper-level impacts reflect a diurnal cycle through the depth of the troposphere. In this study, the possibility of wavelike diurnal responses in tropical cyclones is characterized using 3D cloud-resolving numerical simulations with and without a diurnal cycle. Diurnal waves can only begin to propagate well beyond the storm core, and the outflow region is most receptive to near-core diurnal propagation because of its anticyclonic flow. The tropical cyclone structure appears particularly hostile to diurnal wave propagation during periods when the eyewall experiences a temporary breakdown similar to an eyewall replacement cycle.


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