A cloud-resolving model is used to examine the intensification of tilted tropical cyclones from depression to hurricane strength over relatively cool and warm oceans under idealized conditions where environmental vertical wind shear has become minimal. Variation of the SST does not substantially change the time-averaged relationship between tilt and the radial length scale of the inner core, or between tilt and the azimuthal distribution of precipitation during the hurricane formation period (HFP). By contrast, for systems having similar structural parameters, the HFP lengthens superlinearly in association with a decline of the precipitation rate as the SST decreases from 30° to 26
This study examines two factors impacting initiation of moist deep convection: free-tropospheric environmental relative humidity (
- NSF-PAR ID:
- 10363219
- Publisher / Repository:
- American Meteorological Society
- Date Published:
- Journal Name:
- Journal of the Atmospheric Sciences
- Volume:
- 79
- Issue:
- 2
- ISSN:
- 0022-4928
- Format(s):
- Medium: X Size: p. 337-359
- Size(s):
- ["p. 337-359"]
- Sponsoring Org:
- National Science Foundation
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