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contributor authorKowaleski, Alex M.
contributor authorEvans, Jenni L.
date accessioned2017-06-09T17:33:37Z
date available2017-06-09T17:33:37Z
date copyright2016/10/01
date issued2016
identifier issn0027-0644
identifier otherams-87212.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4230857
description abstractmodified 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.
publisherAmerican Meteorological Society
titleA Reformulation of Tropical Cyclone Potential Intensity Theory Incorporating Energy Production along a Radial Trajectory
typeJournal Paper
journal volume144
journal issue10
journal titleMonthly Weather Review
identifier doi10.1175/MWR-D-15-0383.1
journal fristpage3569
journal lastpage3578
treeMonthly Weather Review:;2016:;volume( 144 ):;issue: 010
contenttypeFulltext


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