Remote Sounding of Cloudy Atmospheres. III. Experimental Verifications

M. T. Chahine Jet Propulsion Laboratory, California Institute of Technology, Pasadena 91103

Search for other papers by M. T. Chahine in
Current site
Google Scholar
PubMed
Close
,
H. H. Aumann Jet Propulsion Laboratory, California Institute of Technology, Pasadena 91103

Search for other papers by H. H. Aumann in
Current site
Google Scholar
PubMed
Close
, and
F. W. Taylor Jet Propulsion Laboratory, California Institute of Technology, Pasadena 91103

Search for other papers by F. W. Taylor in
Current site
Google Scholar
PubMed
Close
Full access

We are aware of a technical issue preventing figures and tables from showing in some newly published articles in the full-text HTML view.
While we are resolving the problem, please use the online PDF version of these articles to view figures and tables.

Abstract

The cloud-filtering technique developed in Parts I and II of this study is experimentally verified in this paper. The verification is based on radiance data measured in the 4.3 and 15 µm bands using a multi-detector sounder mounted on an aircraft. The results presented here show that, from the aircraft height of 7.6 km and in the presence of multiple cloud formations, it is possible to recover simultaneously:

  1. The clear-column atmospheric temperature profile with an rms error of 1 K with respect to radiosondes.

  2. The land and sea surface temperature at all sun zenith angles. The accuracy of the recovered sea-surface temperature is 0.5-1 K with respect to measured bucket temperatures.

  3. The humidity profile (water vapor mixing ratio) with a precision of 10%.

  4. The fractional covers and heights of up to three cloud formations.

  5. The types of clouds, i.e., whether convective or nonconvective.

Abstract

The cloud-filtering technique developed in Parts I and II of this study is experimentally verified in this paper. The verification is based on radiance data measured in the 4.3 and 15 µm bands using a multi-detector sounder mounted on an aircraft. The results presented here show that, from the aircraft height of 7.6 km and in the presence of multiple cloud formations, it is possible to recover simultaneously:

  1. The clear-column atmospheric temperature profile with an rms error of 1 K with respect to radiosondes.

  2. The land and sea surface temperature at all sun zenith angles. The accuracy of the recovered sea-surface temperature is 0.5-1 K with respect to measured bucket temperatures.

  3. The humidity profile (water vapor mixing ratio) with a precision of 10%.

  4. The fractional covers and heights of up to three cloud formations.

  5. The types of clouds, i.e., whether convective or nonconvective.

Save