A reformulation of tropical cyclone potential intensity theory incorporating energy production along a radial trajectory

Alex M. Kowaleski, Jenni Evans

Research output: Contribution to journalArticle

1 Citation (Scopus)

Abstract

A modified formula for calculating tropical cyclone (TC) potential intensity (PI) from a balance between energy production and frictional dissipation in the TC surface layer is developed. This modified formula accounts for energy production and frictional dissipation at multiple radii (and therefore at multiple wind speeds) along the TC inflow trajectory. The PI maximum wind speed values VMAX are calculated using this expanded formula for four canonical radial profiles of wind speed. These results are compared to PI VMAX values calculated using the standard assumption that all energy production and frictional dissipation relevant to maximum intensity occurs at the radius of maximum winds (RMW). The new PI formulation developed here results in PI VMAX values substantially higher than the standard PI VMAX for all four of the radial wind speed profiles examined; the difference is explained by the increase in the outer radial limit of energy production. This increase holds true even if outflow temperature increases with increasing radius, although the VMAX increases with increasing outer radius are somewhat more modest in this case. The extended PI formula yields VMAX values 3-17 m s-1 higher than the standard PI VMAX value when calculated with outer energy production-dissipation limits of 2.0-2.5 RMW, although it yields potentially unrealistic values when calculated with larger outer limits (e.g., 6 RMW). These results are presented as a potential explanation for why individual TCs can exceed their standard PI VMAX values in terms of the storm thermodynamics.

Original languageEnglish (US)
Pages (from-to)3569-3578
Number of pages10
JournalMonthly Weather Review
Volume144
Issue number10
DOIs
StatePublished - Jan 1 2016

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tropical cyclone
trajectory
dissipation
wind velocity
surface layer
inflow
outflow
thermodynamics
energy production
temperature

All Science Journal Classification (ASJC) codes

  • Atmospheric Science

Cite this

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abstract = "A modified formula for calculating tropical cyclone (TC) potential intensity (PI) from a balance between energy production and frictional dissipation in the TC surface layer is developed. This modified formula accounts for energy production and frictional dissipation at multiple radii (and therefore at multiple wind speeds) along the TC inflow trajectory. The PI maximum wind speed values VMAX are calculated using this expanded formula for four canonical radial profiles of wind speed. These results are compared to PI VMAX values calculated using the standard assumption that all energy production and frictional dissipation relevant to maximum intensity occurs at the radius of maximum winds (RMW). The new PI formulation developed here results in PI VMAX values substantially higher than the standard PI VMAX for all four of the radial wind speed profiles examined; the difference is explained by the increase in the outer radial limit of energy production. This increase holds true even if outflow temperature increases with increasing radius, although the VMAX increases with increasing outer radius are somewhat more modest in this case. The extended PI formula yields VMAX values 3-17 m s-1 higher than the standard PI VMAX value when calculated with outer energy production-dissipation limits of 2.0-2.5 RMW, although it yields potentially unrealistic values when calculated with larger outer limits (e.g., 6 RMW). These results are presented as a potential explanation for why individual TCs can exceed their standard PI VMAX values in terms of the storm thermodynamics.",
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A reformulation of tropical cyclone potential intensity theory incorporating energy production along a radial trajectory. / Kowaleski, Alex M.; Evans, Jenni.

In: Monthly Weather Review, Vol. 144, No. 10, 01.01.2016, p. 3569-3578.

Research output: Contribution to journalArticle

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