Vertical temperature profiles were collected from January 6th 2001 to February 26th 2001 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) project of the Italian National Antarctic Research Programme (PNRA) using Sippican T7 Expendable Bathythermograph (XBT). Used probes have a vertical resolution of 65 cm and a maximum nominal depth of 760 m. XBT launches have been interrupted in case of severe sea and weather conditions. This implies the presence of gaps in the sampling. The spatial resolution of the sampling ranges between 15 nm and 20 nm. All temperature profiles are quality controlled for consistency between adjacent profiles and through spike editing. Data are provided in TXT format.

Water temperature from XBT taken from the research vessel Italica in the Southern Ocean and Southwest Pacific Ocean from 2001-01-06 to 2001-02-26 (NCEI Accession 0173213)

Yuri Cotroneo;Giorgio Budillon;Andrea Bergamasco;Massimo De Stefano;Claudia Ferrara;Giancarlo Spezie
2018-01-01

Abstract

Vertical temperature profiles were collected from January 6th 2001 to February 26th 2001 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) project of the Italian National Antarctic Research Programme (PNRA) using Sippican T7 Expendable Bathythermograph (XBT). Used probes have a vertical resolution of 65 cm and a maximum nominal depth of 760 m. XBT launches have been interrupted in case of severe sea and weather conditions. This implies the presence of gaps in the sampling. The spatial resolution of the sampling ranges between 15 nm and 20 nm. All temperature profiles are quality controlled for consistency between adjacent profiles and through spike editing. Data are provided in TXT format.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11367/68910
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