Background
A global-scale circulation carries about 10 or 20 million tons per second of relatively warm water northward into the top kilometer of the North Atlantic Ocean. The water cools off, sinks, and returns southward as a relatively dense flow of "North Atlantic Deep Water " (NADW, see Fig. 1)....
| Main Authors: | , |
|---|---|
| Other Authors: | |
| Format: | Text |
| Language: | English |
| Subjects: | |
| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.597.2791 http://mason.gmu.edu/~bklinger/drake.pdf |
| id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.597.2791 |
|---|---|
| record_format |
openpolar |
| spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.597.2791 2023-05-15T17:13:49+02:00 Background Barry A. Klinger Drake Passage The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.597.2791 http://mason.gmu.edu/~bklinger/drake.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.597.2791 http://mason.gmu.edu/~bklinger/drake.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://mason.gmu.edu/~bklinger/drake.pdf text ftciteseerx 2020-09-06T00:15:58Z A global-scale circulation carries about 10 or 20 million tons per second of relatively warm water northward into the top kilometer of the North Atlantic Ocean. The water cools off, sinks, and returns southward as a relatively dense flow of "North Atlantic Deep Water " (NADW, see Fig. 1). This NADW "overturning " circulation may have an important influence on the climate of Europe, and has been implicated in abrupt climate changes at the end of the last ice age. latitude de pt h (km Text NADW North Atlantic Deep Water North Atlantic Unknown |
| institution |
Open Polar |
| collection |
Unknown |
| op_collection_id |
ftciteseerx |
| language |
English |
| description |
A global-scale circulation carries about 10 or 20 million tons per second of relatively warm water northward into the top kilometer of the North Atlantic Ocean. The water cools off, sinks, and returns southward as a relatively dense flow of "North Atlantic Deep Water " (NADW, see Fig. 1). This NADW "overturning " circulation may have an important influence on the climate of Europe, and has been implicated in abrupt climate changes at the end of the last ice age. latitude de pt h (km |
| author2 |
The Pennsylvania State University CiteSeerX Archives |
| format |
Text |
| author |
Barry A. Klinger Drake Passage |
| spellingShingle |
Barry A. Klinger Drake Passage Background |
| author_facet |
Barry A. Klinger Drake Passage |
| author_sort |
Barry A. Klinger |
| title |
Background |
| title_short |
Background |
| title_full |
Background |
| title_fullStr |
Background |
| title_full_unstemmed |
Background |
| title_sort |
background |
| url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.597.2791 http://mason.gmu.edu/~bklinger/drake.pdf |
| genre |
NADW North Atlantic Deep Water North Atlantic |
| genre_facet |
NADW North Atlantic Deep Water North Atlantic |
| op_source |
http://mason.gmu.edu/~bklinger/drake.pdf |
| op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.597.2791 http://mason.gmu.edu/~bklinger/drake.pdf |
| op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
| _version_ |
1766071010277195776 |