Linear Trends of Temperature at Intermediate and Deep Layers of the North Atlantic and the North Pacific Oceans: 1957–1981Source: Journal of Climate:;1993:;volume( 006 ):;issue: 010::page 1928Author:Antonov, John I.
DOI: 10.1175/1520-0442(1993)006<1928:LTOTAI>2.0.CO;2Publisher: American Meteorological Society
Abstract: Using all available hydrographic station data on ocean temperature observations from World Data Center-B (Obninsk, Russia), investigation of temperature changes in the North Atlantic and North Pacific oceans within the depth range of 300 to 3000 m has been carried out for the period 1957?1981. Results of statistical data analysis show that in the upper layer to about 500-m depths of both oceans, on average, seawater temperature declined. Deeper than 500?600 m in the North Pacific Ocean, no significant temperature changes have been revealed for this 25-year time interval. On average, for the North Atlantic Ocean, a statistically significant temperature rise (about 0.1°C 25 yr?1) is observed in the 800- to 2500-m layer.
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| contributor author | Antonov, John I. | |
| date accessioned | 2017-06-09T15:20:26Z | |
| date available | 2017-06-09T15:20:26Z | |
| date copyright | 1993/10/01 | |
| date issued | 1993 | |
| identifier issn | 0894-8755 | |
| identifier other | ams-4097.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4179478 | |
| description abstract | Using all available hydrographic station data on ocean temperature observations from World Data Center-B (Obninsk, Russia), investigation of temperature changes in the North Atlantic and North Pacific oceans within the depth range of 300 to 3000 m has been carried out for the period 1957?1981. Results of statistical data analysis show that in the upper layer to about 500-m depths of both oceans, on average, seawater temperature declined. Deeper than 500?600 m in the North Pacific Ocean, no significant temperature changes have been revealed for this 25-year time interval. On average, for the North Atlantic Ocean, a statistically significant temperature rise (about 0.1°C 25 yr?1) is observed in the 800- to 2500-m layer. | |
| publisher | American Meteorological Society | |
| title | Linear Trends of Temperature at Intermediate and Deep Layers of the North Atlantic and the North Pacific Oceans: 1957–1981 | |
| type | Journal Paper | |
| journal volume | 6 | |
| journal issue | 10 | |
| journal title | Journal of Climate | |
| identifier doi | 10.1175/1520-0442(1993)006<1928:LTOTAI>2.0.CO;2 | |
| journal fristpage | 1928 | |
| journal lastpage | 1942 | |
| tree | Journal of Climate:;1993:;volume( 006 ):;issue: 010 | |
| contenttype | Fulltext |