A major obstacle in the estimation of windspeed patterns associated with low-altitude windshear with an airborne pulsed Doppler radar system is the presence of strong levels of ground clutter which can strongly bias a windspeed estimate. Typical solutions attempt to remove the clutter energy from the return through clutter rejection filtering. Proposed is a method whereby both the weather and clutter modes present in a return spectrum can be identified to yield an unbiased estimate of the weather mode without the need for clutter rejection filtering. An attempt will be made to show that modeling through a second order extended Prony approach is sufficient for the identification of the weather mode. A pattern recognition approach to windspee...
Atmospheric plume dispersion models are used for a variety of purposes including emergency planning ...
The effects of clutter-rejection filtering on estimating the weather parameters from pulse Doppler r...
An updated NASA atmospheric turbulence model, from 0 to 200 km altitude, which was developed to be m...
Ground clutter interference is a major problem for airborne pulse Doppler radar operating at low alt...
High resolution windspeed profile measurements are needed to provide reliable detection of hazardous...
A 35 km grid limited area mesoscale model was initialized with high density SESAME radiosonde data a...
Investigations were performed to predict the power available from the wind at the Goldstone, Califor...
The small scale wind velocity perturbations in vertical wind profiles at Cape Kennedy, Florida were ...
Wind-borne debris is considered as a major source of damage to civil structures during strong wind s...
Translational state estimation in terminal area operations, using a set of commonly available positi...
A desirable candidate for future weather observation is a polarimetric phased array radar (PPAR), wh...
An analysis is presented for the bivariate parameter differences between the FPS-16 Radar/Jimsphere ...
Improved measurements of precipitation will aid our understanding of the role of latent heating on g...
This document describes the simulation approach used to test the performance of the NASA airborne wi...
The results of a six degree of freedom (6-DOF) nonlinear Monte Carlo dispersion analysis for the lat...
Atmospheric plume dispersion models are used for a variety of purposes including emergency planning ...
The effects of clutter-rejection filtering on estimating the weather parameters from pulse Doppler r...
An updated NASA atmospheric turbulence model, from 0 to 200 km altitude, which was developed to be m...
Ground clutter interference is a major problem for airborne pulse Doppler radar operating at low alt...
High resolution windspeed profile measurements are needed to provide reliable detection of hazardous...
A 35 km grid limited area mesoscale model was initialized with high density SESAME radiosonde data a...
Investigations were performed to predict the power available from the wind at the Goldstone, Califor...
The small scale wind velocity perturbations in vertical wind profiles at Cape Kennedy, Florida were ...
Wind-borne debris is considered as a major source of damage to civil structures during strong wind s...
Translational state estimation in terminal area operations, using a set of commonly available positi...
A desirable candidate for future weather observation is a polarimetric phased array radar (PPAR), wh...
An analysis is presented for the bivariate parameter differences between the FPS-16 Radar/Jimsphere ...
Improved measurements of precipitation will aid our understanding of the role of latent heating on g...
This document describes the simulation approach used to test the performance of the NASA airborne wi...
The results of a six degree of freedom (6-DOF) nonlinear Monte Carlo dispersion analysis for the lat...
Atmospheric plume dispersion models are used for a variety of purposes including emergency planning ...
The effects of clutter-rejection filtering on estimating the weather parameters from pulse Doppler r...
An updated NASA atmospheric turbulence model, from 0 to 200 km altitude, which was developed to be m...