COMPARATIVE STUDY O F OCEANOGRAPHIC CHARACTERISTICS ABOVE/UNDER FIRST-YEAR SEA ICE AT LOW AND HIGH LATITUDES
pump under the first-year ice in the Arctic Ocean " and "the biological processes in Arctic polynya areas", meteorological and oceanographic studies were car-ried out successively at the Saroma KO lagoon, Hokkaido, Japan from Decem-ber 1991 to April 1992, and in Resolute Passage, Cana...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.507.6367 2023-05-15T14:53:35+02:00 COMPARATIVE STUDY O F OCEANOGRAPHIC CHARACTERISTICS ABOVE/UNDER FIRST-YEAR SEA ICE AT LOW AND HIGH LATITUDES Kunio Shirasawa R. Grant In Gram The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.507.6367 http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1995-Shirasawa.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.507.6367 http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1995-Shirasawa.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1995-Shirasawa.pdf text ftciteseerx 2016-01-08T09:27:18Z pump under the first-year ice in the Arctic Ocean " and "the biological processes in Arctic polynya areas", meteorological and oceanographic studies were car-ried out successively at the Saroma KO lagoon, Hokkaido, Japan from Decem-ber 1991 to April 1992, and in Resolute Passage, Canadian Arctic from April to June 1992. Seasonal sea ice at its southern limit in the Sea of Okhotsk reaches a maximum thickness of about 40cm at the Saroma KO lagoon, while ice reaches a maximum thickness of about 2 m in Resolute Passage. In this paper, meteorological and oceanographic variables obtained from both field experi-ments of the SARES project are compared. The presence of sea ice cover leads to major changes in the flow and stratification regime. We observed much weaker currents and the presence of small scale vertical structure in the temperature-salinity regime under complete landfast ice covered areas. It is believed that ice melt and freshwater input from a small river played an important role in generating the observed variability in the lagoon. The presencelabsence of sea ice plays a significant role in determin-ing the oceanographic characteristics of the lagoon and its potential for biolog-ical productivity. It is believed that the difference in solar irradiance between low and high latitudes in seasonally sea-ice covered waters plays a significant role in biological productivity in the spring regime. 1. Text Arctic Arctic Ocean Sea ice ice covered areas ice covered waters Unknown Arctic Arctic Ocean Okhotsk Resolute Passage ENVELOPE(-95.585,-95.585,74.702,74.702) |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
pump under the first-year ice in the Arctic Ocean " and "the biological processes in Arctic polynya areas", meteorological and oceanographic studies were car-ried out successively at the Saroma KO lagoon, Hokkaido, Japan from Decem-ber 1991 to April 1992, and in Resolute Passage, Canadian Arctic from April to June 1992. Seasonal sea ice at its southern limit in the Sea of Okhotsk reaches a maximum thickness of about 40cm at the Saroma KO lagoon, while ice reaches a maximum thickness of about 2 m in Resolute Passage. In this paper, meteorological and oceanographic variables obtained from both field experi-ments of the SARES project are compared. The presence of sea ice cover leads to major changes in the flow and stratification regime. We observed much weaker currents and the presence of small scale vertical structure in the temperature-salinity regime under complete landfast ice covered areas. It is believed that ice melt and freshwater input from a small river played an important role in generating the observed variability in the lagoon. The presencelabsence of sea ice plays a significant role in determin-ing the oceanographic characteristics of the lagoon and its potential for biolog-ical productivity. It is believed that the difference in solar irradiance between low and high latitudes in seasonally sea-ice covered waters plays a significant role in biological productivity in the spring regime. 1. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Kunio Shirasawa R. Grant In Gram |
spellingShingle |
Kunio Shirasawa R. Grant In Gram COMPARATIVE STUDY O F OCEANOGRAPHIC CHARACTERISTICS ABOVE/UNDER FIRST-YEAR SEA ICE AT LOW AND HIGH LATITUDES |
author_facet |
Kunio Shirasawa R. Grant In Gram |
author_sort |
Kunio Shirasawa |
title |
COMPARATIVE STUDY O F OCEANOGRAPHIC CHARACTERISTICS ABOVE/UNDER FIRST-YEAR SEA ICE AT LOW AND HIGH LATITUDES |
title_short |
COMPARATIVE STUDY O F OCEANOGRAPHIC CHARACTERISTICS ABOVE/UNDER FIRST-YEAR SEA ICE AT LOW AND HIGH LATITUDES |
title_full |
COMPARATIVE STUDY O F OCEANOGRAPHIC CHARACTERISTICS ABOVE/UNDER FIRST-YEAR SEA ICE AT LOW AND HIGH LATITUDES |
title_fullStr |
COMPARATIVE STUDY O F OCEANOGRAPHIC CHARACTERISTICS ABOVE/UNDER FIRST-YEAR SEA ICE AT LOW AND HIGH LATITUDES |
title_full_unstemmed |
COMPARATIVE STUDY O F OCEANOGRAPHIC CHARACTERISTICS ABOVE/UNDER FIRST-YEAR SEA ICE AT LOW AND HIGH LATITUDES |
title_sort |
comparative study o f oceanographic characteristics above/under first-year sea ice at low and high latitudes |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.507.6367 http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1995-Shirasawa.pdf |
long_lat |
ENVELOPE(-95.585,-95.585,74.702,74.702) |
geographic |
Arctic Arctic Ocean Okhotsk Resolute Passage |
geographic_facet |
Arctic Arctic Ocean Okhotsk Resolute Passage |
genre |
Arctic Arctic Ocean Sea ice ice covered areas ice covered waters |
genre_facet |
Arctic Arctic Ocean Sea ice ice covered areas ice covered waters |
op_source |
http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1995-Shirasawa.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.507.6367 http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1995-Shirasawa.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766325189069504512 |