All Time Past Year Past 30 Days
Abstract Views 0 0 0
Full Text Views 229 62 24
PDF Downloads 96 40 4

Remote Sensing of Atmospheric Water Vapor and Liquid Water with the Nimbus 5 Microwave Spectrometer

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

Search for other papers by D. H. Staelin in
Current site
Google Scholar
PubMed
Close
,
K. F. KunziResearch Laboratory of Electronics, Massachusetts Institute of Technology, Cambridge, Mass. 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, Mass. 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, Mass. 02139

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

Search for other papers by R. W. Wilcox 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 passive microwave spectrometer on the Nimbus 5 satellite has two channels that measure atmospheric water vapor and liquid water abundances over ocean. Observed water vapor abundances range up to 6 g cm−2 and differ from nearby radiosondes by ∼0.4 g cm−2. Average liquid water abundances over a 300 km observation zone range from −0.01 to 0.2 g cm−2, and have an rms error estimated to be ∼0.01 g cm−2 for most circumstances. These quantitative measurements can be used to construct global maps or to accumulate global statistics.

Abstract

The passive microwave spectrometer on the Nimbus 5 satellite has two channels that measure atmospheric water vapor and liquid water abundances over ocean. Observed water vapor abundances range up to 6 g cm−2 and differ from nearby radiosondes by ∼0.4 g cm−2. Average liquid water abundances over a 300 km observation zone range from −0.01 to 0.2 g cm−2, and have an rms error estimated to be ∼0.01 g cm−2 for most circumstances. These quantitative measurements can be used to construct global maps or to accumulate global statistics.

Save