Related Experiment Video
Updated: May 9, 2026

Scattering And Absorption of Light in Planetary Regoliths
Published on: July 1, 2019
Sensor-based clear and cloud radiance calculations in the community radiative transfer model
Quanhua Liu1, Y Xue, C Li
1Earth System Science Interdisciplinary Center, University of Maryland, College Park, Maryland 20740, USA. qliu123@umd.edu
The Optical Transmittance (OPTRAN) approximation in the Community Radiative Transfer Model (CRTM) enables affordable assimilation of cloudy satellite radiances for improved weather forecasting. This method achieves high accuracy, outperforming the scaling method and supporting operational numerical weather prediction.
Area of Science:
- Atmospheric Science and Meteorology
- Radiative Transfer Modeling
- Satellite Data Assimilation
Background:
- The Community Radiative Transfer Model (CRTM) is crucial for satellite radiance simulations in NOAA's data assimilation systems.
- Assimilation of clear-sky radiances is successful, but cloudy radiances are computationally expensive, hindering severe weather forecasting improvements.
- Current cloud radiance calculations in CRTM are too slow for operational weather forecasting needs.
Purpose of the Study:
- To investigate the accuracy of the Optical Transmittance (OPTRAN) approximation within CRTM for cloudy satellite radiance simulations.
- To assess the feasibility of using OPTRAN-CRTM for affordable assimilation of cloudy radiances in numerical weather prediction.
- To understand the error sources associated with the OPTRAN approximation compared to line-by-line radiative transfer models.
Main Methods:
- Implemented the Optical Transmittance (OPTRAN) band model within CRTM, using cloud optical parameters at band central wavelengths.
- Compared OPTRAN-CRTM cloud radiance calculations against detailed Line-By-Line Radiative Transfer Model (LBLRTM) simulations.
- Evaluated accuracy using data from NOAA's High Resolution Infrared Radiation Sounder/3 (HIRS/3) and Advanced Microwave Sounding Unit (AMSU) sensors.
Main Results:
- OPTRAN-CRTM achieved accuracy better than 0.4 K for infrared (HIRS/3) and 0.1 K for microwave (AMSU) sensors.
- The OPTRAN approximation significantly improves computational efficiency by requiring only one radiative transfer solution per channel.
- The scaling method (SCALING-CRTM) showed larger errors, up to 7 K for HIRS/3 clear-sky and 3.5 K for cloudy conditions.
Conclusions:
- The OPTRAN-CRTM approximation provides adequate accuracy for operational satellite radiance assimilation in numerical forecast models.
- This computationally efficient method makes the assimilation of cloudy radiances affordable, paving the way for improved forecasting.
- OPTRAN-CRTM demonstrates superior performance over the SCALING-CRTM method, particularly under cloudy conditions.
Related Concept Videos
Attenuated Total Reflectance (ATR) Infrared Spectroscopy: Overview
The ATR process begins by directing a beam...
Precipitation Processes
Flame Photometry: Overview
Radiation Pressure: Problem Solving
The average value of the rate of momentum transfer divided by the absorbing area represents the average force per...
Absorption of Radiation
Light Acquisition

