Height-dependent transition from 3-D to 2-D turbulence in the hurricane boundary layer-Reference-Cited by-同舟云学术

Height-dependent transition from 3-D to 2-D turbulence in the hurricane boundary layer

Published:2013-04-12 Issue:7 Volume:40 Page:1439-1442
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Byrne David¹²,Zhang Jun A.³⁴

Affiliation:

1. Institute of Biogeochemistry and Pollutant Dynamics, Department of Environmental; ETH Zürich; Zurich Switzerland

2. Center for Climate Systems Modeling (C2SM), ETH Zürich; Zurich Switzerland

3. National Oceanic and Atmospheric Administration; Atlantic Oceanographic and Meteorological Laboratory, Hurricane Research Division; Miami Florida USA

4. Cooperative Institute for Marine and Atmospheric Studies; University of Miami; Miami Florida USA

Funder

ETH

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference38 articles.

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2. Effects of surface exchange coefficients and turbulence length scales on the intensity and structure of numerically-simulated hurricanes;Bryan;Mon. Wea. Rev.,2012

3. The maximum intensity of tropical cyclones in axisymmetry numerical model simulations;Bryan;Mon. Wea. Rev.,2009

4. Robust inverse energy cascade and turbulence structure in three-dimensional layers of fluid;Byrne;Phys. Fluids,2011

5. Turbulence in more than two and less than three dimensions;Celani;Phys. Rev. Lett.,2010

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