Inversion of Spire NO Data
Abstract
An algorithm was developed to invert spectrally resolved Earth limb radiance profiles. It is applicable in the nonequilibrium altitude regime for species/tangent heights that correspond to the optically thin condition. It was used to infer vertical distributions of temperature and excited NO density from data measured by SPIRE (the Spectral Infrared Rocket Experiment) in the NO fundamental band near 5.3 microns. The solution for excited NO density was used to compute atmospheric radiative cooling rates for the 5.3 microns band and the de-excitation rate constant k0 for the reaction NO + 0 yields NO + 0. The results are in good agreement with previously published values. (Author)
Document Details
- Document Type
- Technical Report
- Publication Date
- Aug 20, 1981
- Accession Number
- ADA108866
Entities
People
- A. S. Zachor
- A. T. Stair Jr.
- R. M. Nadile
- Rajesh Sharma
Organizations
- Boston College