The Ozone Monitoring Instrument
Abstract. A technique for evaluating the radiometric calibration of satellite-born radiometers has been developed utilizing the stable reflectance of the Antarctic land mass. Previously, the scene radiances measured over the Antarctic and Greenland land masses were used to monitor time evolution of...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.614.2621 2023-05-15T14:01:51+02:00 The Ozone Monitoring Instrument G. Jaross J. Warner R. P. Cebula A. Kashlinsky The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.614.2621 http://www.pmodwrc.ch/newrad2005/pdfabstracts/Newrad149.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.614.2621 http://www.pmodwrc.ch/newrad2005/pdfabstracts/Newrad149.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.pmodwrc.ch/newrad2005/pdfabstracts/Newrad149.pdf text ftciteseerx 2016-01-08T14:39:56Z Abstract. A technique for evaluating the radiometric calibration of satellite-born radiometers has been developed utilizing the stable reflectance of the Antarctic land mass. Previously, the scene radiances measured over the Antarctic and Greenland land masses were used to monitor time evolution of sensor radiometric sensitivity and to compare instruments with similar spectral responses. Through the use of radiative transfer modeling, we can now evaluate the albedo calibration (Earth radiance sensitivity divided by solar irradiance sensitivity) of any nadir-viewing, polar orbiting sensor measuring in the 300-800 nm range. Our evaluation of the Ozone Monitoring Instrument on the NASA Aura spacecraft confirms a 2 % calibration uncertainty. Text Antarc* Antarctic Greenland Unknown Antarctic Greenland The Antarctic |
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English |
description |
Abstract. A technique for evaluating the radiometric calibration of satellite-born radiometers has been developed utilizing the stable reflectance of the Antarctic land mass. Previously, the scene radiances measured over the Antarctic and Greenland land masses were used to monitor time evolution of sensor radiometric sensitivity and to compare instruments with similar spectral responses. Through the use of radiative transfer modeling, we can now evaluate the albedo calibration (Earth radiance sensitivity divided by solar irradiance sensitivity) of any nadir-viewing, polar orbiting sensor measuring in the 300-800 nm range. Our evaluation of the Ozone Monitoring Instrument on the NASA Aura spacecraft confirms a 2 % calibration uncertainty. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
G. Jaross J. Warner R. P. Cebula A. Kashlinsky |
spellingShingle |
G. Jaross J. Warner R. P. Cebula A. Kashlinsky The Ozone Monitoring Instrument |
author_facet |
G. Jaross J. Warner R. P. Cebula A. Kashlinsky |
author_sort |
G. Jaross |
title |
The Ozone Monitoring Instrument |
title_short |
The Ozone Monitoring Instrument |
title_full |
The Ozone Monitoring Instrument |
title_fullStr |
The Ozone Monitoring Instrument |
title_full_unstemmed |
The Ozone Monitoring Instrument |
title_sort |
ozone monitoring instrument |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.614.2621 http://www.pmodwrc.ch/newrad2005/pdfabstracts/Newrad149.pdf |
geographic |
Antarctic Greenland The Antarctic |
geographic_facet |
Antarctic Greenland The Antarctic |
genre |
Antarc* Antarctic Greenland |
genre_facet |
Antarc* Antarctic Greenland |
op_source |
http://www.pmodwrc.ch/newrad2005/pdfabstracts/Newrad149.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.614.2621 http://www.pmodwrc.ch/newrad2005/pdfabstracts/Newrad149.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766271909187551232 |