Further Examination of the Thermodynamic Modification of the Inflow Layer of Tropical Cyclones by Vertical Wind Shear

Abstract

Recent work has developed a new framework for the impact of vertical wind shear on the intensity evolution of tropical cyclones. A focus of this framework is on the frustration of the tropical cyclone's power machine by shear-induced persistent downdrafts that flush relatively cool and dry (lower equivalent potential temperature) air into the storm's inflow layer. These previous results have been based on idealised numerical experiments for which we have deliberately chosen a simple set of physical parameterisations. Before efforts are undertaken to test the proposed framework with real atmospheric data, we assess here the robustness of our previous results in a more realistic and representative experimental setup by surveying and diagnosing five additional numerical experiments. The modifications of the experimental setup comprise the values of the exchange coefficients of surface heat and momentum fluxes, the inclusion of experiments with ice microphysics, and the consideration of weaker, but still mature tropical cyclones.

Open PDF

Document Details

Document Type
Technical Report
Publication Date
Jan 11, 2013
Accession Number
ADA573889

Entities

People

  • M. E. Nicholls
  • M. Riemer
  • Michael T. Montgomery

Organizations

  • Naval Postgraduate School

Tags

Communities of Interest

  • Energy and Power Technologies
  • Engineered Resilient Systems

DTIC Thesaurus Topics

  • Boundary Layer
  • Coefficients
  • Convection
  • Cyclones
  • Depression
  • Ecology
  • Energy
  • Heat Energy
  • Heat Of Fusion
  • Intensity
  • Latent Heat
  • Meteorology
  • Momentum
  • Physics
  • Tropical Cyclones
  • Wind
  • Wind Shear

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science/Meteorology
  • Computational Modeling and Simulation
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers