Growth mechanisms of 'Katie's Floeberg'
The growth mechanism of the grounded ice feature on Hanna's Shoal, located at approximately 162 deg W, 72 deg N in the Chukchi Sea, has been analyzed using Landsat I and II satellite imagery. The primary mechanism of growth was deduced to be the formation of large wedges of ice against the upst...
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| Format: | Other/Unknown Material |
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1978
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| Online Access: | http://ntrs.nasa.gov/search.jsp?R=19790066215 |
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ftnasantrs:oai:casi.ntrs.nasa.gov:19790066215 |
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ftnasantrs:oai:casi.ntrs.nasa.gov:19790066215 2023-05-15T15:54:33+02:00 Growth mechanisms of 'Katie's Floeberg' Barrett, S. A. Stringer, W. J. Unclassified, Unlimited, Publicly available JAN 1, 1978 http://ntrs.nasa.gov/search.jsp?R=19790066215 unknown http://ntrs.nasa.gov/search.jsp?R=19790066215 Accession ID: 79A50228 Copyright Other Sources 43 Arctic and Alpine Research; 10; 4, 19; 1978 1978 ftnasantrs 2012-02-15T13:56:53Z The growth mechanism of the grounded ice feature on Hanna's Shoal, located at approximately 162 deg W, 72 deg N in the Chukchi Sea, has been analyzed using Landsat I and II satellite imagery. The primary mechanism of growth was deduced to be the formation of large wedges of ice against the upstream edge of the feature. These wedges of piled ice form in three stages and may or may not become permanently affixed to the core of the feature. Remains of these growth patterns can sometimes be seen in the interior of the feature on the satellite imagery. Other/Unknown Material Chukchi Chukchi Sea NASA Technical Reports Server (NTRS) Chukchi Sea |
| institution |
Open Polar |
| collection |
NASA Technical Reports Server (NTRS) |
| op_collection_id |
ftnasantrs |
| language |
unknown |
| topic |
43 |
| spellingShingle |
43 Barrett, S. A. Stringer, W. J. Growth mechanisms of 'Katie's Floeberg' |
| topic_facet |
43 |
| description |
The growth mechanism of the grounded ice feature on Hanna's Shoal, located at approximately 162 deg W, 72 deg N in the Chukchi Sea, has been analyzed using Landsat I and II satellite imagery. The primary mechanism of growth was deduced to be the formation of large wedges of ice against the upstream edge of the feature. These wedges of piled ice form in three stages and may or may not become permanently affixed to the core of the feature. Remains of these growth patterns can sometimes be seen in the interior of the feature on the satellite imagery. |
| format |
Other/Unknown Material |
| author |
Barrett, S. A. Stringer, W. J. |
| author_facet |
Barrett, S. A. Stringer, W. J. |
| author_sort |
Barrett, S. A. |
| title |
Growth mechanisms of 'Katie's Floeberg' |
| title_short |
Growth mechanisms of 'Katie's Floeberg' |
| title_full |
Growth mechanisms of 'Katie's Floeberg' |
| title_fullStr |
Growth mechanisms of 'Katie's Floeberg' |
| title_full_unstemmed |
Growth mechanisms of 'Katie's Floeberg' |
| title_sort |
growth mechanisms of 'katie's floeberg' |
| publishDate |
1978 |
| url |
http://ntrs.nasa.gov/search.jsp?R=19790066215 |
| op_coverage |
Unclassified, Unlimited, Publicly available |
| geographic |
Chukchi Sea |
| geographic_facet |
Chukchi Sea |
| genre |
Chukchi Chukchi Sea |
| genre_facet |
Chukchi Chukchi Sea |
| op_source |
Other Sources |
| op_relation |
http://ntrs.nasa.gov/search.jsp?R=19790066215 Accession ID: 79A50228 |
| op_rights |
Copyright |
| _version_ |
1766389782421700608 |