S. Roland Drayson

TL;DR: The Halogen Occultation Experiment (HALOE) uses solar occultation to measure vertical profiles of O3, HCl, HF, CH4, H2O, NO, NO2, aerosol extinction, and temperature versus pressure with an instantaneous vertical field of view of 1.6 km at the earth limb.

TL;DR: The HALogen Occultation Experiment (HALOE) instrument on UARS observes vertical profiles of ozone and other gases of interest for atmospheric chemistry using the solar occultation technique as discussed by the authors.

TL;DR: In the LIMS experiment using thermal IR limb scanning to sound the composition and structure of the upper atmosphere, one of the channels was spectrally centered at 6.9 micrometers to measure the vertical profile and global distribution of stratospheric water vapor as discussed by the authors.

TL;DR: The validation of results from the nitrogen dioxide channel and the quality of the data are examined in connection with the LIMS experiment which ran from late October 1978 to late May 1979.

TL;DR: HALOE observations of O3, CH4, HF, H2O, NO, NO2, and HCl collected during the October 1991 Antarctic spring period are reported in this paper.