Surface Topography of the Greenland Ice Sheet from Satellite Radar Altimetry PDF Download
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Author: Publisher: ISBN: Category : Greenland Languages : en Pages : 114
Book Description
This document describes the process of production of maps of the surface of the Greenland ice sheet from data from remote sensing by a Seasat satellite, and defines ice flow directions, together with maps of the Jakobshavn Glacier drainage and the ice divide near Crete Station.
Author: Publisher: ISBN: Category : Greenland Languages : en Pages : 114
Book Description
This document describes the process of production of maps of the surface of the Greenland ice sheet from data from remote sensing by a Seasat satellite, and defines ice flow directions, together with maps of the Jakobshavn Glacier drainage and the ice divide near Crete Station.
Author: Publisher: ISBN: Category : Greenland Languages : en Pages : 120
Book Description
This document describes the process of production of maps of the surface of the Greenland ice sheet from data from remote sensing by a Seasat satellite, and defines ice flow directions, together with maps of the Jakobshavn Glacier drainage and the ice divide near Crete Station.
Author: R. L. Brooks Publisher: ISBN: Category : Languages : en Pages : 5
Book Description
Analysis of data collected from geodynamics experimental ocean satellite (GEOS 3) equipped with radar altimeter permits elevation of Greenland ice sheet surface to be determined to accuracy of plus or minus 2 m and surface features of ice flow to be delineated.
Author: Craig S. Lingle Publisher: ISBN: Category : Languages : en Pages : 8
Book Description
Mean changes in the surface elevation near the west margin of the Greenland ice sheet are measured using Seasat altimetry and altimetry from the Geosat Exact Repeat Mission (ERM). The Seasat data extend from early July through early October 1978. The ERM data extend from winter 1986-87 through fall 1988. Both seasonal and multi-year changes are measured using altimetry referenced to GEM T2 orbits. The possible effects of orbit error are minimized by adjusting the orbits into a common ocean surface. Seasonal mean changes in the surface height are recognizable during the Geosat ERM. The multi-year measurements indicate the surface was lower by 0.4 +/- 0.4 m on average in late summer 1987 than in late summer 1978. The surface was lower by 0.2 +/- 0.5 m on average in late summer 1988 than in late summer 1978. As a control case, the computations are also carried out using altimetry referenced to orbits not adjusted into a common ocean surface.
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Author: Robert A. Bindschadler
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Author: ![Surface Topography of the Greenland Ice Sheet Form [i.e. From] Satelilite [sic] Radar Altimetry PDF](https://books.google.com/books/content/images/frontcover/1qF7swEACAAJ?fife=w80-h100)
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Author: R. L. Brooks
Author: Diana M. Segura
Author: Craig S. Lingle