A measurement of the albedo of thick cirrus clouds at 3.9 microns

Cirrus (ice) clouds are often semitransparent (transmittance greater than zero, but less than one), which makes it difficult to measure fundamental cloud properties, such as albedo. This paper explores a way to measure the albedo of thick cirrus clouds (zero transmittance) at 3.9 microns using GOES...

Full description

Saved in:
Bibliographic Details
Published inGeophysical research letters Vol. 29; no. 10; pp. 9 - 1 to 9-3
Main Author Kidder, S Q
Format Journal Article
LanguageEnglish
Published 15.05.2002
Online AccessGet full text

Cover

Loading…
More Information
Summary:Cirrus (ice) clouds are often semitransparent (transmittance greater than zero, but less than one), which makes it difficult to measure fundamental cloud properties, such as albedo. This paper explores a way to measure the albedo of thick cirrus clouds (zero transmittance) at 3.9 microns using GOES Imager data. In brief, the 10.7-micron GOES data are used to separate the cirrus clouds into temperature classes. Then the measured 3.9-micron radiance is plotted against the cosine of the solar zenith angle. A theoretical relationship between radiance and solar zenith angle is used to extract the albedo. The result is that thick cirrus clouds have an albedo of 1.08 +/- 0.05 percent at 3.9 microns. The albedo of thick cirrus is a step toward the measurement of the transmittance of thin cirrus. (Author)
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
content type line 23
ObjectType-Feature-1
ISSN:0094-8276