1975
DOI: 10.1016/0011-7471(75)90077-7
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On the flow of water out of the Weddell Sea

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Cited by 132 publications
(135 citation statements)
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“…As well as feeding the world's oceans by circulating cold bottom water, the Weddell Sea produces some of the coldest deep waters in the world. Weddell Sea Bottom Water is highly influential in the Weddell and Scotia Seas as a stable, dense and extreme cold water mass as low as -1.88°C (Carmack and Foster, 1975;Fahrbach et al, 1995;Smith et al, 1999). Flowing west into the Scotia Sea, bottom water acts as an important counter current to the powerful Antarctic Circumpolar Current.…”
Section: Discussionmentioning
confidence: 99%
“…As well as feeding the world's oceans by circulating cold bottom water, the Weddell Sea produces some of the coldest deep waters in the world. Weddell Sea Bottom Water is highly influential in the Weddell and Scotia Seas as a stable, dense and extreme cold water mass as low as -1.88°C (Carmack and Foster, 1975;Fahrbach et al, 1995;Smith et al, 1999). Flowing west into the Scotia Sea, bottom water acts as an important counter current to the powerful Antarctic Circumpolar Current.…”
Section: Discussionmentioning
confidence: 99%
“…28, which captures the full range of WDW. WDW is characterized having a potential temperature of more than 0 • C and salinity of more than 34.6 (Carmack and Foster, 1975) or, taking a more conservative approach, neutral density limits of 28 to 28.27 kg m −3 . Figure 28a shows good general agreement with the T − S diagram of Fig.…”
Section: Water Mass Properties Of the Weddell Gyre Along The Prime Mementioning
confidence: 99%
“…2, WSDW is characterised by a potential temperature (y) in the range À0:7oyo0:21C and salinity (S) below 34.70. y ¼ À0:71C was chosen by Carmack and Foster (1975) to differentiate between WSDW, which can overflow the South Solid lines represent neutral density contours at selected water mass boundaries. As neutral density is not only a function of temperature and salinity (but also of pressure, latitude and longitude) these contours are computed by fitting second order polynomials to the entire ALBATROSS data set.…”
Section: The Deep Water Masses Of the Scotia Seamentioning
confidence: 99%