Accuracy of RT code SORD for realistic atmospheric profiles

Date

2016-12-14

Department

Program

Citation of Original Publication

Korkin, Sergey, Alexei Lyapustin, Aliaksandr Sinyuk, and Brent Holben. “Accuracy of RT Code SORD for Realistic Atmospheric Profiles.” In Remote Sensing of Clouds and the Atmosphere XXI, 10001:73–84. SPIE, 2016. https://doi.org/10.1117/12.2241411.

Rights

THIS WORK WAS WRITTEN AS PART OF ONE OF THE AUTHOR'S OFFICIAL DUTIES AS AN EMPLOYEE OF THE UNITED STATES GOVERNMENT AND IS THEREFORE A WORK OF THE UNITED STATES GOVERNMENT. IN ACCORDANCE WITH 17 U.S.C. 105, NO COPYRIGHT PROTECTION IS AVAILABLE FOR SUCH WORKS UNDER U.S. LAW.
PUBLIC DOMAIN

Subjects

Abstract

We discuss accuracy of our recently developed RT code SORD using 2 benchmark scenarios published by the IPRT group in 2015. These scenarios define atmospheres with a complicate dependence of scattering and absorption properties over height (profile). Equal step, dh=1km, is assumed in the profiles. We developed subroutines that split such atmospheres into layers of the same optical thickness, dτ. We provide full text of the subroutines with comments in Appendix. The dτ is a step for vertical integration in the method of successive orders. Modification of the input profiles from “equal step over h” to “equal step over τ” changes input for RT simulations. This may cause errors at or above the acceptable level of the measurement uncertainty. We show errors of the RT code SORD for both intensity and polarization. In addition to that, using our discrete ordinates RT code IPOL, we discuss one more IPRT scenario, in which changes in height profile indeed cause unacceptable errors. Clear understanding of source and magnitude of these errors is important, e.g. for the AERONET retrieval algorithm.