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Cooling and ventilating the abyssal ocean.
Orsi, A., Jacobs, S., Gordon, A. and Visbeck, Martin (2001) Cooling and ventilating the abyssal ocean. Geophysical Research Letters, 28 . pp. 2923-2926. DOI 10.1029/2001GL012830.
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Abstract
The abyssal ocean is filled with cold, dense waters that sink along the Antarctic continental slope and overflow sills that lie south of the Nordic Seas. Recent integrations of chlorofluorocarbon‐11 (CFC) measurements are similar in Antarctic Bottom Water (AABW) and in lower North Atlantic Deep Water (NADW), but Antarctic inputs are ≈ 2°C colder than their northern counterparts. This indicates comparable ventilation rates from both polar regions, and accounts for the Southern Ocean dominance over abyssal cooling. The decadal CFC‐based estimates of recent ventilation are consistent with other hydrographic observations and with longer‐term radiocarbon data, but not with hypotheses of a 20th‐century slowdown in the rate of AABW formation. Significant variability is not precluded by the available ocean measurements, however, and interannual to decadal changes are increasingly evident at high latitudes.
Document Type: | Article |
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Keywords: | abyssal ocean, cooling, ventilating |
Refereed: | Yes |
Open Access Journal?: | No |
Publisher: | AGU (American Geophysical Union) |
Date Deposited: | 18 Feb 2008 17:25 |
Last Modified: | 14 Feb 2018 09:03 |
URI: | https://oceanrep.geomar.de/id/eprint/1609 |
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