Abstract
Simulation of infrared radiance fluctuations in the upper atmosphere depends on fluctuations in atmospheric species number densities, vibrational state populations, and the kinetic temperatures along the sensor line-of-sight (LOS). The model developed in this paper predicts the two-dimensional radiance covariance using linearized equations to connect atmospheric temperature fluctuations and LOS radiance fluctuations. The SHARC1 model is used to calculate mean LOS radiance values and radiance derivatives which are necessary to determine the radiance statistics. The radiance statistics are non-stationary and are explicitly bandpass and sensor FOV dependent.
© 1995 Optical Society of America
PDF ArticleMore Like This
FW Taylor
ThB1 Optical Remote Sensing of the Atmosphere (ORS) 1990
Shepard A. Clough
TuB5 Optical Remote Sensing of the Atmosphere (ORS) 1995
P. Varanasi, V. Nemtchinov, and Z. Li
TuB3 Optical Remote Sensing of the Atmosphere (ORS) 1995