TABLE 1. Depth and location of ice cores Core Location Depth (m)
~ , ABSTRACT. ln spring 1983 work on the ice shelves of northern Ellesmere lsland was continued. A total of 55 m of 7.6 cm diameter ice core was ob-tained from 10 locations. The longest core of 31.79 m is composed of iced-firn and basement ice and can be divided into three distinct strata accord-ing...
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.583.1926 http://pubs.aina.ucalgary.ca/arctic/Arctic38-3-174.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.583.1926 2023-05-15T14:19:40+02:00 TABLE 1. Depth and location of ice cores Core Location Depth (m) Ward Hunt Wh/ Basement Ice Ice Shelf The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.583.1926 http://pubs.aina.ucalgary.ca/arctic/Arctic38-3-174.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.583.1926 http://pubs.aina.ucalgary.ca/arctic/Arctic38-3-174.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic38-3-174.pdf Total 55.00 text ftciteseerx 2016-08-28T00:04:10Z ~ , ABSTRACT. ln spring 1983 work on the ice shelves of northern Ellesmere lsland was continued. A total of 55 m of 7.6 cm diameter ice core was ob-tained from 10 locations. The longest core of 31.79 m is composed of iced-firn and basement ice and can be divided into three distinct strata accord-ing to ice salinity. Oscillating strains in Ward Hunt Ice Shelf were measured with a wire strainmeter. It is suggested that the periodic calving of ice from Ward Hunt Ice Shelf might be related to the effects of the high frequency oscillation of 35s to 40s. Ice conditions along 150 km of coastline con-i tinue to change. Continued monitoring of the ice shelves and landfast ice is believed to be necessary in view of the offshore development in the Beaufort Sea. Text Arctic Beaufort Sea ice core Ice Shelf Ice Shelves Ward Hunt Ice Shelf Unknown Ward Hunt Ice Shelf ENVELOPE(-73.499,-73.499,83.122,83.122) |
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ftciteseerx |
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English |
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Total 55.00 |
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Total 55.00 Ward Hunt Wh/ Basement Ice Ice Shelf TABLE 1. Depth and location of ice cores Core Location Depth (m) |
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Total 55.00 |
| description |
~ , ABSTRACT. ln spring 1983 work on the ice shelves of northern Ellesmere lsland was continued. A total of 55 m of 7.6 cm diameter ice core was ob-tained from 10 locations. The longest core of 31.79 m is composed of iced-firn and basement ice and can be divided into three distinct strata accord-ing to ice salinity. Oscillating strains in Ward Hunt Ice Shelf were measured with a wire strainmeter. It is suggested that the periodic calving of ice from Ward Hunt Ice Shelf might be related to the effects of the high frequency oscillation of 35s to 40s. Ice conditions along 150 km of coastline con-i tinue to change. Continued monitoring of the ice shelves and landfast ice is believed to be necessary in view of the offshore development in the Beaufort Sea. |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
| author |
Ward Hunt Wh/ Basement Ice Ice Shelf |
| author_facet |
Ward Hunt Wh/ Basement Ice Ice Shelf |
| author_sort |
Ward Hunt |
| title |
TABLE 1. Depth and location of ice cores Core Location Depth (m) |
| title_short |
TABLE 1. Depth and location of ice cores Core Location Depth (m) |
| title_full |
TABLE 1. Depth and location of ice cores Core Location Depth (m) |
| title_fullStr |
TABLE 1. Depth and location of ice cores Core Location Depth (m) |
| title_full_unstemmed |
TABLE 1. Depth and location of ice cores Core Location Depth (m) |
| title_sort |
table 1. depth and location of ice cores core location depth (m) |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.583.1926 http://pubs.aina.ucalgary.ca/arctic/Arctic38-3-174.pdf |
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ENVELOPE(-73.499,-73.499,83.122,83.122) |
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Ward Hunt Ice Shelf |
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Ward Hunt Ice Shelf |
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Arctic Beaufort Sea ice core Ice Shelf Ice Shelves Ward Hunt Ice Shelf |
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Arctic Beaufort Sea ice core Ice Shelf Ice Shelves Ward Hunt Ice Shelf |
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http://pubs.aina.ucalgary.ca/arctic/Arctic38-3-174.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.583.1926 http://pubs.aina.ucalgary.ca/arctic/Arctic38-3-174.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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