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The magnitude and diurnal variation of observed wave variance are used to constrain the momentum fluxes as a function of height and time.
The influence of sea environment parameters and operational profiles including the use of different scatter diagrams, and wave variance spectra have been analyzed.
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In this paper we examine the possibility of using the wave variances in the MLT to estimate the momentum flux spectrum near the source height in the troposphere.
Observations of MF radar winds made at Christmas Island (2∘N, 157∘W) between 1990 and 1997 are used to produce daily values of gravity wave variances in the equatorial mesosphere and lower thermosphere (70 100 km).
This paper provides further observational constraints to tide-sensitive variables (H2O, O3, and gravity wave variances) used by the models, which are obtained simultaneously by upper atmosphere research satellite microwave limb sounder at altitudes below the MLT region.
Recently, Venkateswara Rao et al. (2012b) reported correlations between short-period gravity-wave variances at the mesopause and the strength of the MSAO observed using an MF radar in Indonesia.
If we use the observation data including the S waves, the variance between observations and synthetics will be determined almost exclusively by the fitting of the S waves (i.e., the fitting of the P wave and PP waves is of minimal importance for the variance).
For a plane wave, the Rytov variance is calculated as σ ln I R 2 = ln I - ln I 2 = 1.
Using data collected by the AMPTE-UKS satellite on 21st September , 1984 this paper investigates the nature of these waves using the variance analysis technique to determine the polarisation and maximum/minimum variance directions.
Our work presents an analysis of optimal values of correction zones and an optimal position of the center of the reference sphere based on the variance of wave aberration for the image quality evaluation.
Current methods of generating stationary random fields having power-law spectra are based on fast Fourier transforming an array of random numbers with zero mean and unit variance to wave space.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com