Iceberg Motion in Lancaster Sound
the movement of icebergs in eastern Lancaster Sound and northwestern Baffin Bay. Data were recorded by photographing the radar screen every 20 minutes. Meteorological measurements were also made. The data were processed by computer to provide a statistical picture of the iceberg motions as well as t...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.489.6130 2023-05-15T14:19:40+02:00 Iceberg Motion in Lancaster Sound The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.489.6130 http://pubs.aina.ucalgary.ca/arctic/Arctic35-1-219.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.489.6130 http://pubs.aina.ucalgary.ca/arctic/Arctic35-1-219.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic35-1-219.pdf Key words iceberg motion radar tracking Baffin Bay Lancaster Sound text ftciteseerx 2016-01-08T08:23:25Z the movement of icebergs in eastern Lancaster Sound and northwestern Baffin Bay. Data were recorded by photographing the radar screen every 20 minutes. Meteorological measurements were also made. The data were processed by computer to provide a statistical picture of the iceberg motions as well as tracks of individual bergs. The mean circulation pattern of the ice was well defined and variations about the mean did not greatly change the general form of the pattern. The dominant feature of the flow was a stream of icebergs moving with a mean speed of about 40 cm s " southward along the east coast of Devon Island from north of Philpots Island to Cape Sherard and then westward to Cape Warrénder. At Cape Warrender, the bergs turned toward the centre of Lancaster Sound with directions ranging from southwest to southeast and average speeds up to 50 cm s-'. East of the coastal stream in Baffin Bay, the icebergs moved slowly (<25 cm s-I) westward tojoin the coastal stream, while south of the stream at the entrance to Lancaster Sound two large persistent eddies were observed. In Baffin Bay, variations in the flow field appeared to be in response to direct meteorological forcing while in Lancaster Sound no evidence of this response was found. The variations in iceberg motion in the sound appeared to be caused by changes in the currents. Text Arctic Baffin Bay Baffin Bay Baffin Devon Island Lancaster Sound Unknown Baffin Bay Cape Sherard ENVELOPE(-80.222,-80.222,74.600,74.600) Cape Warrender ENVELOPE(-81.759,-81.759,74.471,74.471) Devon Island ENVELOPE(-88.000,-88.000,75.252,75.252) Lancaster Sound ENVELOPE(-83.999,-83.999,74.218,74.218) Philpots Island ENVELOPE(-79.886,-79.886,74.924,74.924) |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
topic |
Key words iceberg motion radar tracking Baffin Bay Lancaster Sound |
spellingShingle |
Key words iceberg motion radar tracking Baffin Bay Lancaster Sound Iceberg Motion in Lancaster Sound |
topic_facet |
Key words iceberg motion radar tracking Baffin Bay Lancaster Sound |
description |
the movement of icebergs in eastern Lancaster Sound and northwestern Baffin Bay. Data were recorded by photographing the radar screen every 20 minutes. Meteorological measurements were also made. The data were processed by computer to provide a statistical picture of the iceberg motions as well as tracks of individual bergs. The mean circulation pattern of the ice was well defined and variations about the mean did not greatly change the general form of the pattern. The dominant feature of the flow was a stream of icebergs moving with a mean speed of about 40 cm s " southward along the east coast of Devon Island from north of Philpots Island to Cape Sherard and then westward to Cape Warrénder. At Cape Warrender, the bergs turned toward the centre of Lancaster Sound with directions ranging from southwest to southeast and average speeds up to 50 cm s-'. East of the coastal stream in Baffin Bay, the icebergs moved slowly (<25 cm s-I) westward tojoin the coastal stream, while south of the stream at the entrance to Lancaster Sound two large persistent eddies were observed. In Baffin Bay, variations in the flow field appeared to be in response to direct meteorological forcing while in Lancaster Sound no evidence of this response was found. The variations in iceberg motion in the sound appeared to be caused by changes in the currents. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
Iceberg Motion in Lancaster Sound |
title_short |
Iceberg Motion in Lancaster Sound |
title_full |
Iceberg Motion in Lancaster Sound |
title_fullStr |
Iceberg Motion in Lancaster Sound |
title_full_unstemmed |
Iceberg Motion in Lancaster Sound |
title_sort |
iceberg motion in lancaster sound |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.489.6130 http://pubs.aina.ucalgary.ca/arctic/Arctic35-1-219.pdf |
long_lat |
ENVELOPE(-80.222,-80.222,74.600,74.600) ENVELOPE(-81.759,-81.759,74.471,74.471) ENVELOPE(-88.000,-88.000,75.252,75.252) ENVELOPE(-83.999,-83.999,74.218,74.218) ENVELOPE(-79.886,-79.886,74.924,74.924) |
geographic |
Baffin Bay Cape Sherard Cape Warrender Devon Island Lancaster Sound Philpots Island |
geographic_facet |
Baffin Bay Cape Sherard Cape Warrender Devon Island Lancaster Sound Philpots Island |
genre |
Arctic Baffin Bay Baffin Bay Baffin Devon Island Lancaster Sound |
genre_facet |
Arctic Baffin Bay Baffin Bay Baffin Devon Island Lancaster Sound |
op_source |
http://pubs.aina.ucalgary.ca/arctic/Arctic35-1-219.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.489.6130 http://pubs.aina.ucalgary.ca/arctic/Arctic35-1-219.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766291438142750720 |