4.7 Article

Organized kinetic energy backscatter in the hurricane boundary layer from radar measurements

Journal

JOURNAL OF FLUID MECHANICS
Volume 924, Issue -, Pages -

Publisher

CAMBRIDGE UNIV PRESS
DOI: 10.1017/jfm.2021.632

Keywords

turbulent boundary layers; vortex dynamics; atmospheric flows

Funding

  1. NOAA Weather Program Office [NA19OAR4590329]

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Hurricanes rely heavily on boundary layer energetics, with large-scale organized backscatter and interactions between adjacent eddies impacting vortex dynamics. Stress tensor components play a key role in the alternating scatter structure, and sub-filter-scale energy transfer has a significant impact on kinetic energy budgets in the hurricane boundary layer.
The fluid mechanics of hurricanes strongly depends on boundary layer energetics due to the warm-core nature of the system with peak velocities located at lower levels. One barrier that has inhibited a more complete characterization of energy transfer in the boundary layer is a lack of observations that resolve large, turbulent eddies. In particular, the occurrence and structure of upscale energy transfer (backscatter) in the hurricane boundary layer as well as the effects of backscatter on the vortex intensity are unknown. The analysis presented here of very high-resolution, three-dimensional wind observations from Hurricane Rita (2005) at peak intensity reveals large regions of organized backscatter in the boundary layer associated with coherent, turbulent eddies. Strong forwardscatter is also found next to the backscatter regions due to the interaction between adjacent eddies. Two components of the stress tensor are primarily responsible for this alternating scatter structure, as shown by large correlation coefficients between the fields: the radial-vertical component (tau(13)) and the azimuthal-vertical component (tau(23)) with average correlations of 79% and 49 %, respectively. The Leonard, Reynolds and cross-term stress components are also provided. The impact of the sub-filter-scale energy transfer is estimated by computing the kinetic energy budget for the resolved-scale and eddy-scale motions. The results show that the sub-filter-scale energy transfer term is of the same order as the other terms in the eddy-scale budgets, contributing between 16% and 40% to the local time tendency with an average contribution of approximately 30 %. These results indicate that the coherent turbulent eddies can affect the vortex dynamics through wave-wave nonlinear interactions, which can subsequently influence the wave-mean flow interactions. This is the first study to examine the full sub-filter-scale energy transfer and its impact on the kinetic energy budget in the hurricane boundary layer. These findings emphasize the importance of coherent turbulence in the energy cascade and have the potential to improve turbulence closure schemes used in numerical simulations.

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