Potential temperature, oxygen and circulation of bottom water
Abstract--The circulation of bottom and near-bottom water can be determined in a qualitative manner by inspecting parameter distributions. Bottom potentia! temperature and oxygen (which show a definite relation in the t~-Oz diagram) are very useful for this purpose in the portion of the Southern Oce...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.452.9653 2023-05-15T16:02:29+02:00 Potential temperature, oxygen and circulation of bottom water Arnold L. Gordon The Pennsylvania State University CiteSeerX Archives 1966 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.452.9653 http://www.ldeo.columbia.edu/~agordon/publications/Gordon_AntBottomWater_DSR66.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.452.9653 http://www.ldeo.columbia.edu/~agordon/publications/Gordon_AntBottomWater_DSR66.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ldeo.columbia.edu/~agordon/publications/Gordon_AntBottomWater_DSR66.pdf text 1966 ftciteseerx 2016-01-08T06:00:09Z Abstract--The circulation of bottom and near-bottom water can be determined in a qualitative manner by inspecting parameter distributions. Bottom potentia! temperature and oxygen (which show a definite relation in the t~-Oz diagram) are very useful for this purpose in the portion of the Southern Ocean dealt with in this paper (20°W westward to 170°W and south of 50°S). Observations u ed are deeper than 3000 m and within 300 m of the bottom. There are two areas of cold water (< 0.0°C): the more extreme manating from the Weddell Sea and the other from the Ross Sea. The Weddell Sea Bottom Water flows to the east of the South Sandwich Trench into the Argentine Basin, though some water does enter the trench and flows north-ward. The bottom waters of the Scotia Sea come from between the 3000-3200 mlevel of the Weddell Sea through a passage at 39°W in the South Orkney Ridge. A tongue of this water flows into the southern Drake Passage, confining to the northern Drake Passage the warmer bottom water from the Pacific Ocean. This warmer bottom water forms a rapid easterly current which enters the South Atlantic west of Shag Rocks. The cold Scotia Sea bottom water does not penetrate he Pacific Ocean but is topographically or dynamically restrained. Circulation in the eastern Scotia Sea is weak to moderate. Text Drake Passage Ross Sea Scotia Sea Southern Ocean Weddell Sea Unknown Argentine Drake Passage Pacific Ross Sea Scotia Sea Shag Rocks ENVELOPE(-42.033,-42.033,-53.550,-53.550) South Sandwich Trench ENVELOPE(-25.000,-25.000,-56.500,-56.500) Southern Ocean Weddell Weddell Sea |
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Open Polar |
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ftciteseerx |
language |
English |
description |
Abstract--The circulation of bottom and near-bottom water can be determined in a qualitative manner by inspecting parameter distributions. Bottom potentia! temperature and oxygen (which show a definite relation in the t~-Oz diagram) are very useful for this purpose in the portion of the Southern Ocean dealt with in this paper (20°W westward to 170°W and south of 50°S). Observations u ed are deeper than 3000 m and within 300 m of the bottom. There are two areas of cold water (< 0.0°C): the more extreme manating from the Weddell Sea and the other from the Ross Sea. The Weddell Sea Bottom Water flows to the east of the South Sandwich Trench into the Argentine Basin, though some water does enter the trench and flows north-ward. The bottom waters of the Scotia Sea come from between the 3000-3200 mlevel of the Weddell Sea through a passage at 39°W in the South Orkney Ridge. A tongue of this water flows into the southern Drake Passage, confining to the northern Drake Passage the warmer bottom water from the Pacific Ocean. This warmer bottom water forms a rapid easterly current which enters the South Atlantic west of Shag Rocks. The cold Scotia Sea bottom water does not penetrate he Pacific Ocean but is topographically or dynamically restrained. Circulation in the eastern Scotia Sea is weak to moderate. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Arnold L. Gordon |
spellingShingle |
Arnold L. Gordon Potential temperature, oxygen and circulation of bottom water |
author_facet |
Arnold L. Gordon |
author_sort |
Arnold L. Gordon |
title |
Potential temperature, oxygen and circulation of bottom water |
title_short |
Potential temperature, oxygen and circulation of bottom water |
title_full |
Potential temperature, oxygen and circulation of bottom water |
title_fullStr |
Potential temperature, oxygen and circulation of bottom water |
title_full_unstemmed |
Potential temperature, oxygen and circulation of bottom water |
title_sort |
potential temperature, oxygen and circulation of bottom water |
publishDate |
1966 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.452.9653 http://www.ldeo.columbia.edu/~agordon/publications/Gordon_AntBottomWater_DSR66.pdf |
long_lat |
ENVELOPE(-42.033,-42.033,-53.550,-53.550) ENVELOPE(-25.000,-25.000,-56.500,-56.500) |
geographic |
Argentine Drake Passage Pacific Ross Sea Scotia Sea Shag Rocks South Sandwich Trench Southern Ocean Weddell Weddell Sea |
geographic_facet |
Argentine Drake Passage Pacific Ross Sea Scotia Sea Shag Rocks South Sandwich Trench Southern Ocean Weddell Weddell Sea |
genre |
Drake Passage Ross Sea Scotia Sea Southern Ocean Weddell Sea |
genre_facet |
Drake Passage Ross Sea Scotia Sea Southern Ocean Weddell Sea |
op_source |
http://www.ldeo.columbia.edu/~agordon/publications/Gordon_AntBottomWater_DSR66.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.452.9653 http://www.ldeo.columbia.edu/~agordon/publications/Gordon_AntBottomWater_DSR66.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766398145782087680 |