作者: Kenneth J. Voss , Howard R. Gordon , Yuntao Ge
DOI: 10.1117/12.140647
关键词:
摘要: ABSTRACT It is demonstrated that Fraunhofer lines in the solar spectrum will be filled by inelastic scattering ocean. The relative depth of a line, ij, defined as ratio irradiance at center line to background continuum, can then used measure amount light field,i.e., measuring contributions elastic and processes field deduced. An oceanographic instrument was developed in-sifti utilizes 1 m monochrometer, CCD camera, two collectors with fiber optic guide. Results preliminaryfield measurements are presented discussed. 1. INTRODUCTION Oceanic increasingly being postulated important sources underwater butuntil now no direct these ambient conditions have been reported.It has demonstrated, theoretically, Raman play significant role radiative transfer