The drift of ice island WH-5
ABSTRACT. From 1962 to 1964 Ice Island WH-5 drifted south from the Arctic Ocean water transport through Nares Strait is not continuous, and during the summer of 1963 was through Nares Strait and Baffin Bay. The movements of WH-5 indicate that the southward clockwise gyre in Kane Basin. By the time t...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.567.2504 2023-05-15T14:19:44+02:00 The drift of ice island WH-5 David C. Nutt Ml Nponubob The Pennsylvania State University CiteSeerX Archives 1966 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.567.2504 http://pubs.aina.ucalgary.ca/arctic/Arctic19-3-244.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.567.2504 http://pubs.aina.ucalgary.ca/arctic/Arctic19-3-244.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic19-3-244.pdf text 1966 ftciteseerx 2016-01-08T12:19:03Z ABSTRACT. From 1962 to 1964 Ice Island WH-5 drifted south from the Arctic Ocean water transport through Nares Strait is not continuous, and during the summer of 1963 was through Nares Strait and Baffin Bay. The movements of WH-5 indicate that the southward clockwise gyre in Kane Basin. By the time they reached the waters of Labfador and Newfound-interrupted by pulses of surface water to the north and the development of a sluggish counter-land in 1964 the WH-5 pieces were extensively scattered due to their Irregular escape from Smith Sound and the vagaries of the Baffin and Labrador Current systems. Rl%UMl?. La Ddrive de I’île de glace WH-5. De 1962 à 1964, l’île de lace WH-5 a dCrivC vers le sud, de l’ocCan Arctique à travers le dCtroit de Nares et la baie de Bakn. Les mouvements continu et que durant 1 ” de 1963, il fut interrompu par des poussCes d’eau de surface vers le de WH-5 indiquent que le transport d’eau vers le sud à travers le dCtroit de Nares n’est pas atteignirent les eaux du Labrador et de Terre-Neuve en 1964, les dCbris de WH-5 ava!ent kt6 nord et le dCveloppement d’un lent mouvement lCvogyre dans le bassin de Kane. Lorsqu’ils considCrablement dispersCs par leur sortie irrkgulière du dCtrolt de Smith et les caprlces des systèmes de courants de Baffin et du Labrador. Text Arctic Arctic Arctic Ocean Arctique* Baffin Bay Baffin Bay Baffin Kane Basin Nares strait Smith sound Terre-Neuve Unknown Arctic Arctic Ocean Baffin Bay Kane ENVELOPE(-63.038,-63.038,-73.952,-73.952) Lent ENVELOPE(-66.783,-66.783,-66.867,-66.867) Nares ENVELOPE(158.167,158.167,-81.450,-81.450) Smith Sound ENVELOPE(-73.996,-73.996,78.419,78.419) |
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Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
ABSTRACT. From 1962 to 1964 Ice Island WH-5 drifted south from the Arctic Ocean water transport through Nares Strait is not continuous, and during the summer of 1963 was through Nares Strait and Baffin Bay. The movements of WH-5 indicate that the southward clockwise gyre in Kane Basin. By the time they reached the waters of Labfador and Newfound-interrupted by pulses of surface water to the north and the development of a sluggish counter-land in 1964 the WH-5 pieces were extensively scattered due to their Irregular escape from Smith Sound and the vagaries of the Baffin and Labrador Current systems. Rl%UMl?. La Ddrive de I’île de glace WH-5. De 1962 à 1964, l’île de lace WH-5 a dCrivC vers le sud, de l’ocCan Arctique à travers le dCtroit de Nares et la baie de Bakn. Les mouvements continu et que durant 1 ” de 1963, il fut interrompu par des poussCes d’eau de surface vers le de WH-5 indiquent que le transport d’eau vers le sud à travers le dCtroit de Nares n’est pas atteignirent les eaux du Labrador et de Terre-Neuve en 1964, les dCbris de WH-5 ava!ent kt6 nord et le dCveloppement d’un lent mouvement lCvogyre dans le bassin de Kane. Lorsqu’ils considCrablement dispersCs par leur sortie irrkgulière du dCtrolt de Smith et les caprlces des systèmes de courants de Baffin et du Labrador. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
David C. Nutt Ml Nponubob |
spellingShingle |
David C. Nutt Ml Nponubob The drift of ice island WH-5 |
author_facet |
David C. Nutt Ml Nponubob |
author_sort |
David C. Nutt |
title |
The drift of ice island WH-5 |
title_short |
The drift of ice island WH-5 |
title_full |
The drift of ice island WH-5 |
title_fullStr |
The drift of ice island WH-5 |
title_full_unstemmed |
The drift of ice island WH-5 |
title_sort |
drift of ice island wh-5 |
publishDate |
1966 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.567.2504 http://pubs.aina.ucalgary.ca/arctic/Arctic19-3-244.pdf |
long_lat |
ENVELOPE(-63.038,-63.038,-73.952,-73.952) ENVELOPE(-66.783,-66.783,-66.867,-66.867) ENVELOPE(158.167,158.167,-81.450,-81.450) ENVELOPE(-73.996,-73.996,78.419,78.419) |
geographic |
Arctic Arctic Ocean Baffin Bay Kane Lent Nares Smith Sound |
geographic_facet |
Arctic Arctic Ocean Baffin Bay Kane Lent Nares Smith Sound |
genre |
Arctic Arctic Arctic Ocean Arctique* Baffin Bay Baffin Bay Baffin Kane Basin Nares strait Smith sound Terre-Neuve |
genre_facet |
Arctic Arctic Arctic Ocean Arctique* Baffin Bay Baffin Bay Baffin Kane Basin Nares strait Smith sound Terre-Neuve |
op_source |
http://pubs.aina.ucalgary.ca/arctic/Arctic19-3-244.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.567.2504 http://pubs.aina.ucalgary.ca/arctic/Arctic19-3-244.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766291473537433600 |