Abstract
Quantitative interpretation of remote sensing measurements of aerosols requires knowledge of the interaction of small particles with electromagnetic radiation. Many natural particles are known to have nonspherical shapes, and scattering properties of such particles can differ both quantitatively and qualitatively from those of “equivalent” spheres, thereby significantly affecting the results of remote sensing retrievals. In this paper, we calculate the distribution of intensity of electromagnetic radiation inside prolate spheroidal silicate particles and compared them with analogous results for spherical particles.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: Journal of Quantitative Spectroscopy and Radiative Transfer
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
