The effects of the Arctic haze as determined from airborne radiometric measurements during AGASP II

• Main Authors: Valero, Francisco P. J., Ackerman, Thomas P., Gore, Warren J. Y.
• Format: Other/Unknown Material
• Language: unknown
• Published: 1989
• Subjects: 45; Arctic; albedo
• Online Access: http://ntrs.nasa.gov/search.jsp?R=19900037583

The effect of the Arctic-haze aerosol on the parameters of solar radiation was investigated using airborne radiometric measurements of radiation parameters during the second Arctic Gas and Aerosol Sampling Project. Simultaneously with absorption measurements, optical depths and total, direct, and scattered radiation fields were determined. The experimentally determined parameters were used to define an aerosol model, which was then used to calculate atmospheric heating rate profiles. It was found that, besides the increased absorption (30 to 40 percent) and scattering of radiation by the atmosphere, Arctic haze reduces the surface absorption of solar energy by 6 to 10 percent, and the effective planetary albedo over ice surfaces by 3 to 6 percent.