Tropical cyclone-relative environmental helicity and the pathways to intensification in shear

Matthew J. Onderlinde, David S Nolan

Research output: Contribution to journalArticle

15 Citations (Scopus)

Abstract

Tropical cyclone-relative environmental helicity (TCREH) is a measure of how the wind vector changes direction with height, and it has been shown to modulate the rate at which tropical cyclones (TCs) develop both in idealized simulations and in reanalysis data. The channels through which this modulation occurs remain less clear. This study aims to identify the mechanisms that lead to the observed variations in intensification rate. Results suggest that the difference in intensification rate between TCs embedded in positive versus negative TCREH primarily results from the position of convection and associated latent heat fluxes relative to the wind shear vector. When TCREH is positive, convection is more readily advected upshear and air parcels that experience larger fluxes are more frequently ingested into the TC core. Trajectories computed from high-resolution simulations demonstrate the recovery of equivalent potential temperature downwind of convection, latent heat flux near the TC core, and parcel routes through updrafts in convection. Differences in trajectory characteristics between TCs embedded in positive versus negative TCREH are presented. Contoured frequency-by-altitude diagrams (CFADs) show that convection is distributed differently around TCs embedded in environments characterized by positive versus negative TCREH. They also show that the nature of the most intense convection differs only slightly between cases of positive and negative TCREH. The results of this study emphasize the fact that significant variability in TC-intensification rate results from vertical variations in the environmental wind direction, even when the 850-200-hPa wind shear vector remains unchanged.

Original languageEnglish (US)
Pages (from-to)869-890
Number of pages22
JournalJournal of the Atmospheric Sciences
Volume73
Issue number2
DOIs
StatePublished - 2016

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tropical cyclone
convection
wind shear
latent heat flux
trajectory
updraft
potential temperature
wind direction
simulation
diagram

Keywords

  • Atm/ocean structure/phenomena
  • Hurricanes/typhoons
  • Mesoscale models
  • Models and modeling
  • Physical meteorology and climatology
  • Tropical cyclones

ASJC Scopus subject areas

  • Atmospheric Science

Cite this

Tropical cyclone-relative environmental helicity and the pathways to intensification in shear. / Onderlinde, Matthew J.; Nolan, David S.

In: Journal of the Atmospheric Sciences, Vol. 73, No. 2, 2016, p. 869-890.

Research output: Contribution to journalArticle

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