Horizontal wavenumber spectra of winds, temperature, and trace gases during the Pacific Exploratory Missions: 2. Gravity waves, quasi-two-dimensional turbulence, and vortical modes
Name
Choetal-1999JGR2.pdf
Size
1.27 MB
Format
Adobe PDF
Checksum (MD5)
76ec937830c0b636dcf9c294245a7ada
Author(s) • •
Barrick, John D.
Cho, John Y. N.
Newell, Reginald E.
Date Issued
July 1999
Journal
Journal of Geophysical Research: Atmospheres
Publisher
American Geophysical Union (AGU)
Citation
Cho, John Y. N. et al. “Horizontal Wavenumber Spectra of Winds, Temperature, and Trace Gases During the Pacific Exploratory Missions: 2. Gravity Waves, Quasi-Two-Dimensional Turbulence, and Vortical Modes.” Journal of Geophysical Research: Atmospheres 104, D13 (July 1999): 16297–16308 © 1999 American Geophysical Union
Version
Final published version
Abstract
We examine the horizontal wavenumber spectra of horizontal velocity and potential temperature collected by aircraft above the Pacific Ocean to determine whether gravity waves, quasi-two-dimensional (Q-2-D) turbulence, or vortical modes dominate atmospheric fluctuations at scale sizes of 1–100 km and altitudes of 2–12 km. We conclude from the study of Doppler-shifting effects that Q-2-D turbulence and/or vortical modes are more prevalent than gravity waves over the ocean, except in the equatorial zone. The results are consistent with recent numerical simulations of Q-2-D turbulence, which show that the characteristic inverse cascade of energy is greatly facilitated by the presence of background rotation. Furthermore, a Stokes-parameter analysis reveals the general paucity of coherent wavelike motions, although specific cases of gravity-wave propagation are observed. Finally, a case study of a long flight segment displays a k⁻³ horizontal velocity variance spectrum at scales longer than about 100 km. A Stokes-parameter analysis indicates that these large-scale fluctuations were likely due to vortical modes rather than inertio-gravity waves.
MIT Department
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Terms of Use
Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.
Persistent DSpace Link
DOI of Published Version
https://doi.org/10.1029/1999JD900068