ICESat's Laser Measurements of Polar Ice, Atmosphere, Ocean, and Land

The Ice, Cloud and Land Elevation Satellite (ICESat) mission will measure changes in elevation of the Greenland and Antarctic ice sheets as part of NASA's Earth Observing System (EOS) of satellites. Time-series of elevation changes will enable determination of the present-day mass balance of th...

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Main Authors: Koblinsky, Chester J., Abshire, J., Hancock, D., Dezio, J., Zwally, H. J., Schutz, B., Abdalati, W., Brenner, A., Bentley, C., Bufton, J., Harding, D.
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Published: 2001
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Online Access:http://hdl.handle.net/2060/20010097344
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record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:20010097344 2023-05-15T13:47:44+02:00 ICESat's Laser Measurements of Polar Ice, Atmosphere, Ocean, and Land Koblinsky, Chester J. Abshire, J. Hancock, D. Dezio, J. Zwally, H. J. Schutz, B. Abdalati, W. Brenner, A. Bentley, C. Bufton, J. Harding, D. Unclassified, Unlimited, Publicly available [2001] application/pdf http://hdl.handle.net/2060/20010097344 unknown Document ID: 20010097344 http://hdl.handle.net/2060/20010097344 No Copyright CASI Geosciences (General) 2001 ftnasantrs 2019-08-31T23:07:21Z The Ice, Cloud and Land Elevation Satellite (ICESat) mission will measure changes in elevation of the Greenland and Antarctic ice sheets as part of NASA's Earth Observing System (EOS) of satellites. Time-series of elevation changes will enable determination of the present-day mass balance of the ice sheets, study of associations between observed ice changes and polar climate, and estimation of the present and future contributions of the ice sheets to global sea level rise. Other scientific objectives of ICESat include: global measurements of cloud heights and the vertical structure of clouds and aerosols; precise measurements of land topography and vegetation canopy heights; and measurements of sea ice roughness, sea ice thickness, ocean surface elevations, and surface reflectivity. The Geoscience Laser Altimeter System (GLAS) on ICESat has a 1064 nm laser channel for surface altimetry and dense cloud heights and a 532 nm lidar channel for the vertical distribution of clouds and aerosols. The accuracy of surface ranging is 10 cm, averaged over 60 m diameter laser footprints spaced at 172 m along-track. The orbital altitude will be around 600 km at an inclination of 94 deg with a 183-day repeat pattern. The onboard GPS receiver will enable radial orbit determinations to better than 5 cm, and star-trackers will enable footprints to be located to 6 m horizontally. The spacecraft attitude will be controlled to point the laser beam to within +/- 35 m of reference surface tracks at high latitudes. ICESat is designed to operate for 3 to 5 years and should be followed by successive missions to measure ice changes for at least 15 years. Other/Unknown Material Antarc* Antarctic Greenland Sea ice NASA Technical Reports Server (NTRS) Antarctic Greenland
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic Geosciences (General)
spellingShingle Geosciences (General)
Koblinsky, Chester J.
Abshire, J.
Hancock, D.
Dezio, J.
Zwally, H. J.
Schutz, B.
Abdalati, W.
Brenner, A.
Bentley, C.
Bufton, J.
Harding, D.
ICESat's Laser Measurements of Polar Ice, Atmosphere, Ocean, and Land
topic_facet Geosciences (General)
description The Ice, Cloud and Land Elevation Satellite (ICESat) mission will measure changes in elevation of the Greenland and Antarctic ice sheets as part of NASA's Earth Observing System (EOS) of satellites. Time-series of elevation changes will enable determination of the present-day mass balance of the ice sheets, study of associations between observed ice changes and polar climate, and estimation of the present and future contributions of the ice sheets to global sea level rise. Other scientific objectives of ICESat include: global measurements of cloud heights and the vertical structure of clouds and aerosols; precise measurements of land topography and vegetation canopy heights; and measurements of sea ice roughness, sea ice thickness, ocean surface elevations, and surface reflectivity. The Geoscience Laser Altimeter System (GLAS) on ICESat has a 1064 nm laser channel for surface altimetry and dense cloud heights and a 532 nm lidar channel for the vertical distribution of clouds and aerosols. The accuracy of surface ranging is 10 cm, averaged over 60 m diameter laser footprints spaced at 172 m along-track. The orbital altitude will be around 600 km at an inclination of 94 deg with a 183-day repeat pattern. The onboard GPS receiver will enable radial orbit determinations to better than 5 cm, and star-trackers will enable footprints to be located to 6 m horizontally. The spacecraft attitude will be controlled to point the laser beam to within +/- 35 m of reference surface tracks at high latitudes. ICESat is designed to operate for 3 to 5 years and should be followed by successive missions to measure ice changes for at least 15 years.
author Koblinsky, Chester J.
Abshire, J.
Hancock, D.
Dezio, J.
Zwally, H. J.
Schutz, B.
Abdalati, W.
Brenner, A.
Bentley, C.
Bufton, J.
Harding, D.
author_facet Koblinsky, Chester J.
Abshire, J.
Hancock, D.
Dezio, J.
Zwally, H. J.
Schutz, B.
Abdalati, W.
Brenner, A.
Bentley, C.
Bufton, J.
Harding, D.
author_sort Koblinsky, Chester J.
title ICESat's Laser Measurements of Polar Ice, Atmosphere, Ocean, and Land
title_short ICESat's Laser Measurements of Polar Ice, Atmosphere, Ocean, and Land
title_full ICESat's Laser Measurements of Polar Ice, Atmosphere, Ocean, and Land
title_fullStr ICESat's Laser Measurements of Polar Ice, Atmosphere, Ocean, and Land
title_full_unstemmed ICESat's Laser Measurements of Polar Ice, Atmosphere, Ocean, and Land
title_sort icesat's laser measurements of polar ice, atmosphere, ocean, and land
publishDate 2001
url http://hdl.handle.net/2060/20010097344
op_coverage Unclassified, Unlimited, Publicly available
geographic Antarctic
Greenland
geographic_facet Antarctic
Greenland
genre Antarc*
Antarctic
Greenland
Sea ice
genre_facet Antarc*
Antarctic
Greenland
Sea ice
op_source CASI
op_relation Document ID: 20010097344
http://hdl.handle.net/2060/20010097344
op_rights No Copyright
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