Meteorology and Atmospheric Physics

, Volume 65, Issue 3, pp 233–240

Dissipative heating and hurricane intensity

  • M. Bister
  • K. A. Emanuel
Article

DOI: 10.1007/BF01030791

Cite this article as:
Bister, M. & Emanuel, K.A. Meteorl. Atmos. Phys. (1998) 65: 233. doi:10.1007/BF01030791

Summary

Dissipative heating has not been accounted for in either numerical simulations of hurricanes or in theories for the maximum intensity of hurricanes. We argue that the bulk of dissipative heating occurs in the atmospheric boundary layer near the radius of maximum winds and, using both theory and numerical simulation, show that dissipative heating increases maximum wind speeds in tropical cyclones by about 20%.

Copyright information

© Springer-Verlag 1998

Authors and Affiliations

  • M. Bister
    • 1
  • K. A. Emanuel
    • 1
  1. 1.Program in Atmospheres, Oceans, and ClimateMassachusetts Institute of TechnologyCambridgeU.S.A.