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Position of main ACC fronts south of New Zealand from satellite altimetry and XB...
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Water temperature data from XBT taken from the research vessel Italica in the So...
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Water temperature from XBT taken from research vessel Italica in the Southern Oc...
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Water temperature from XBT taken from the research vessel Italica in the Souther...
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Water temperature from XBT taken from the research vessel Italica in the Souther...
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Water temperature from XBT taken from the research vessel Italica in the Souther...
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Water temperature from XBT taken from the research vessel Italica in the Souther...
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Water temperature data from XBT collected from research vessel Italica in Southe...
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Water temperature from XBT taken from the research vessel Italica in the Souther...
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Water temperature from XBT taken from the research vessel Italica in the Souther...
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Water temperature data from XBT taken from the research vessel Italica in the So...
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Water temperature from XBT taken from the research vessel Italica in the Souther...
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Water temperature from XBT taken from the research vessel Italica in the Souther...
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Water temperature data from XBT taken from research vessel Italica in the Southe...
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Water temperature from XBT taken from research vessel Italica in the Southern Oc...
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Water temperature from XBT taken from the research vessel Italica in the Souther...
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Vertical temperature profiles were taken in January 2010 from the research vessel Italica during an oceanographic cruise between New Zealand and the Ross Sea in the framework of the Climatic Long Term Interaction for the Mass-balance in Antarctica (CLIMA) phase IV project of the Italian National Antarctic Research Programme (PNRA) using Sippican T7 Expendable Bathythermograph (XBT) with a vertical resolution of 65 cm and a maximum nominal depth of 760 m. Ship speed lower than 15 kn allows the probe to reach about 900 m depth. The transects were completed during 5 days to provide a synoptic picture of the thermal structure of the upper Southern Ocean. A regular 15 nm spatial sampling rate was adopted across the frontal regions of the Antarctic Circumpolar Current. All temperature profiles are quality controlled for consistency between adjacent profiles and by spike editing. Data are in TXT format
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