Abstract

Using Clementine data, the phase curves of the lunar surface were investigated at small phase angles (0° to 10°) by direct comparison with standard phase angle (30°) data. We found the geological type dependence and wavelength dependence of the phase curve. Additionally, we found a negative correlation between the reflectance at standard phase angle 30° and the brightness ratio I( small phase angle) I(30°) . The dependencies on the terrain type and wavelength can be simply approximated by the dependence on the reflectance.

Full Text
Paper version not known

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 call

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.