资源环境科技发展态势分析平台

We examine the characteristics of secondary gravity waves (GWs) excited by a localized (in space) and intermittent (in time) body force in the atmosphere. This force is a horizontal acceleration of the background flow created when primary GWs dissipate and deposit their momentum on spatial and temporal scales of the wave packet. A broad spectrum of secondary GWs is excited with horizontal scales much larger than that of the primary GW. The polarization relations cause the temperature spectrum of the secondary GWs generally to peak at larger intrinsic periods (Ir) and horizontal wavelengths (H) than the vertical velocity spectrum. We find that the one-dimensional spectra (with regard to frequency or wave number) follow lognormal distributions. We show that secondary GWs can be identified by a horizontally displaced observer as fishbone or > structures in z - t plots whereby the positive and negative GW phase lines meet at the knee, z(knee), which is the altitude of the force center. We present two wintertime cases of lidar temperature measurements at McMurdo, Antarctica (166.69 degrees E, 77.84 degrees S) whereby fishbone structures are seen with z(knee)=43 and 52km. We determine the GW parameters and density-weighted amplitudes for each. We show that these parameters are similar below and above z(knee). We verify that the GWs with upward (downward) phase progression are downward (upward) propagating via use of model background winds. We conclude that these GWs are likely secondary GWs having ground-based periods (r)=6-10hr and vertical wavelengths (z)=6-14km, and that they likely propagate primarily southward.