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- W2015827844 abstract "Abstract Current measurements and serial temperature and salinity observations made in McMurdo Sound during the 1960–61 summer are presented. Most of the current measurements were at two sites close to Cape Armitage, the southern extremity of Ross Island;; these show a residual current of about half a knot flowing towards the Ross Ice Shelf from McMurdo Sound, the fastest currents being close to the sea bottom. Harmonic constants were calculated for the tidal current components. The data are used as a basis for estimating the annual heat and mass transport associated with the southward flow of sea water across a boundary at latitude 77° 50°S. Thermal energy amounting to 7–4 X 1017 calories, available for melting ice, is estimated to be transported across the boundary during the first quarter of each year, the transport at other times being small. A volume of 2–7 X 1013 m3 yr–1 is estimated to be transported annually across the boundary, with little seasonal variation in the transport rate." @default.
- W2015827844 created "2016-06-24" @default.
- W2015827844 creator A5032786188 @default.
- W2015827844 date "1963-06-01" @default.
- W2015827844 modified "2023-09-24" @default.
- W2015827844 title "Hydrological heat and mass transport across the boundary of the ice shelf in Mcmurdo sound, Antarctica" @default.
- W2015827844 cites W1652918156 @default.
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- W2015827844 doi "https://doi.org/10.1080/00288306.1963.10422072" @default.
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