I. Temperatures of polar ice deposits on mercury and the moon. II. Jovian atmospheric dynamics from Galileo imaging
<p>Locations on Mercury that produce ice-like radar responses lie within impact craters that have very cold, permanently shaded floors. The retention of possible ice deposits is determined largely by their temperature. We present model- calculated temperatures of flat surfaces and surfaces...
Internet
https://thesis.library.caltech.edu/7447/1/Vasavada_ar_1998.pdfVasavada, Ashwin R. (1998) I. Temperatures of polar ice deposits on mercury and the moon. II. Jovian atmospheric dynamics from Galileo imaging. Dissertation (Ph.D.), California Institute of Technology. doi:10.7907/ps1y-d710. https://resolver.caltech.edu/CaltechTHESIS:01282013-083854060 <https://resolver.caltech.edu/CaltechTHESIS:01282013-083854060>