Answers are grounded in this paper and cite their sources.
The correlation signals of the incoherent, quasi-coherent, and coherent backscatterings from clouds have been analytically calculated from a unified formalism based on the Eulerian description for a generic weather radar with pulse-pair function, especially aiming for a space-/airborne mission. The spectral broadening due to Doppler fading and wind shears is calculated from this formalism. Since the coupling of these two effects in the spectral broadening is substantial, a conventional estimation is found not to be adapted for the space-/airborne radar. The condition of pulse-pair interval to make data treatment of this operation correspond to that of the fast Fourier transform (FFT) operation is also derived. Further, comparing the derivation of the quasi-coherent scattering to that of the incoherent scattering within the unified formalism, as concerns the Fraunhofer region, it is proven that the former scattering can be represented in a similar form to the latter one, even for nonuniformly illuminated clouds, despite the difference in scattering properties. In addition, the reestimation of the volumetric reflectivity for the quasi-coherent scattering is performed. Finally, the Doppler correlation signals for the coherent backscattering and for the optical partial reflection from a keen boundary of cloud density are formulated.
No takes yet. Share an insight, caveat, or question.
S. Kobayashi (2002) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: