All Time Past Year Past 30 Days
Abstract Views 0 0 0
Full Text Views 148 15 0
PDF Downloads 26 2 0

Microwave Atmospheric Temperature Sounding: Effects of Clouds on the Nimbus 5 Satellite Data

D. H. StaelinResearch Laboratory of Electronics, Massachusetts Institute of Technology, Cambridge 02139

Search for other papers by D. H. Staelin in
Current site
Google Scholar
PubMed
Close
,
A. L. CasselResearch Laboratory of Electronics, Massachusetts Institute of Technology, Cambridge 02139

Search for other papers by A. L. Cassel in
Current site
Google Scholar
PubMed
Close
,
K. F. KunziResearch Laboratory of Electronics, Massachusetts Institute of Technology, Cambridge 02139

Search for other papers by K. F. Kunzi in
Current site
Google Scholar
PubMed
Close
,
R. L. PettyjohnResearch Laboratory of Electronics, Massachusetts Institute of Technology, Cambridge 02139

Search for other papers by R. L. Pettyjohn in
Current site
Google Scholar
PubMed
Close
,
R. K. L. PoonResearch Laboratory of Electronics, Massachusetts Institute of Technology, Cambridge 02139

Search for other papers by R. K. L. Poon in
Current site
Google Scholar
PubMed
Close
,
P. W. RosenkranzResearch Laboratory of Electronics, Massachusetts Institute of Technology, Cambridge 02139

Search for other papers by P. W. Rosenkranz in
Current site
Google Scholar
PubMed
Close
, and
J. W. WatersJet Propulsion Laboratory, California Institute of Technology, Pasadena 91103

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

Abstract

The microwave spectrometer on the Nimbus 5 earth observatory satellite has been used to measure thermal radiation in five frequency bands between 22.235 and 58.8 GHz. Clouds were observed to affect less than 0.5% of the temperature profile soundings. Most such effects occur in the intertropical convergence zone and alter the inferred temperature profile by less than a few degrees Centigrade. These effects are evident as cold spots at 53.65 GHz and can be identified by virtue of their small spatial extent, in contrast to smooth variations characteristic of normal atmospheric temperature fields. These effects at 53.65 GHz are sufficiently well correlated with inferred liquid water abundances that they can be used for detecting major storm systems over both land and sea.

Abstract

The microwave spectrometer on the Nimbus 5 earth observatory satellite has been used to measure thermal radiation in five frequency bands between 22.235 and 58.8 GHz. Clouds were observed to affect less than 0.5% of the temperature profile soundings. Most such effects occur in the intertropical convergence zone and alter the inferred temperature profile by less than a few degrees Centigrade. These effects are evident as cold spots at 53.65 GHz and can be identified by virtue of their small spatial extent, in contrast to smooth variations characteristic of normal atmospheric temperature fields. These effects at 53.65 GHz are sufficiently well correlated with inferred liquid water abundances that they can be used for detecting major storm systems over both land and sea.

Save