Arid
报告编号NASA-CR-168799, NAS 1.26:168799, AR-00
来源IDNTRS_Document_ID: 19820014955
Theoretical and lidar studies of the density response of the mesospheric sodium layer to gravity wave perturbations
Shelton, J. D.; Gardner, C. S.
英文摘要The density response of atmospheric layers to gravity waves is developed in two forms, an exact solution and a perturbation series solution. The degree of nonlinearity in the layer density response is described by the series solution whereas the exact solution gives insight into the nature of the responses. Density perturbation in an atmospheric layer are shown to be substantially greater than the atmospheric density perturbation associated with the propagation of a gravity wave. Because of the density gradients present in atmospheric layers, interesting effects were observed such as a phase reversal in the linear layer response which occurs near the layer peak. Once the layer response is understood, the sodium layer can be used as a tracer of atmospheric wave motions. A two dimensional digital signal processing technique was developed. Both spatial and temporal filtering are utilized to enhance the resolution by decreasing shot noise by more han 10 dB. Many of the features associated with a layer density response to gravity waves were observed in high resolution density profiles of the mesospheric sodium layer. These include nonlinearities as well as the phase reversal in the linear layer response.
英文关键词DENSITY MEASUREMENT GRAVITY WAVES MESOSPHERE OPTICAL RADAR AERONOMY SIGNAL PROCESSING SODIUM STRATOSPHERE VARIABILITY
出版年1981
报告类型Technical Report
语种英语
国家美国
URLhttp://hdl.handle.net/2060/19820014955
资源类型科技报告
条目标识符http://119.78.100.177/qdio/handle/2XILL650/258897
推荐引用方式
GB/T 7714
Shelton, J. D.,Gardner, C. S.. Theoretical and lidar studies of the density response of the mesospheric sodium layer to gravity wave perturbations,1981.
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