About uncertainties in practical salinity calculations

In the current state of the art, salinity is a quantity computed from conductivity ratio measurements, with temperature and pressure known at the time of the measurement, and using the Practical Salinity Scale algorithm of 1978 (PSS-78). This calculation gives practical salinity values <I&...

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Main Author: M. Le Menn
Format: Article
Language:English
Published: Copernicus Publications 2011-10-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/7/651/2011/os-7-651-2011.pdf
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spelling doaj-3a671dfe9031413a898e0ac59525ea962020-11-24T21:28:35ZengCopernicus PublicationsOcean Science1812-07841812-07922011-10-017565165910.5194/os-7-651-2011About uncertainties in practical salinity calculationsM. Le MennIn the current state of the art, salinity is a quantity computed from conductivity ratio measurements, with temperature and pressure known at the time of the measurement, and using the Practical Salinity Scale algorithm of 1978 (PSS-78). This calculation gives practical salinity values <I>S</I>. The uncertainty expected in PSS-78 values is ±0.002, but no details have ever been given on the method used to work out this uncertainty, and the error sources to include in this calculation. Following a guide published by the Bureau International des Poids et Mesures (BIPM), using two independent methods, this paper assesses the uncertainties of salinity values obtained from a laboratory salinometer and Conductivity-Temperature-Depth (CTD) measurements after laboratory calibration of a conductivity cell. The results show that the part due to the PSS-78 relations fits is sometimes as significant as the instrument's. This is particularly the case with CTD measurements where correlations between variables contribute mainly to decreasing the uncertainty of <I>S</I>, even when expanded uncertainties of conductivity cell calibrations are for the most part in the order of 0.002 mS cm<sup>−1</sup>. The relations given here, and obtained with the normalized GUM method, allow a real analysis of the uncertainties' sources and they can be used in a more general way, with instruments having different specifications.http://www.ocean-sci.net/7/651/2011/os-7-651-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Le Menn
spellingShingle M. Le Menn
About uncertainties in practical salinity calculations
Ocean Science
author_facet M. Le Menn
author_sort M. Le Menn
title About uncertainties in practical salinity calculations
title_short About uncertainties in practical salinity calculations
title_full About uncertainties in practical salinity calculations
title_fullStr About uncertainties in practical salinity calculations
title_full_unstemmed About uncertainties in practical salinity calculations
title_sort about uncertainties in practical salinity calculations
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2011-10-01
description In the current state of the art, salinity is a quantity computed from conductivity ratio measurements, with temperature and pressure known at the time of the measurement, and using the Practical Salinity Scale algorithm of 1978 (PSS-78). This calculation gives practical salinity values <I>S</I>. The uncertainty expected in PSS-78 values is ±0.002, but no details have ever been given on the method used to work out this uncertainty, and the error sources to include in this calculation. Following a guide published by the Bureau International des Poids et Mesures (BIPM), using two independent methods, this paper assesses the uncertainties of salinity values obtained from a laboratory salinometer and Conductivity-Temperature-Depth (CTD) measurements after laboratory calibration of a conductivity cell. The results show that the part due to the PSS-78 relations fits is sometimes as significant as the instrument's. This is particularly the case with CTD measurements where correlations between variables contribute mainly to decreasing the uncertainty of <I>S</I>, even when expanded uncertainties of conductivity cell calibrations are for the most part in the order of 0.002 mS cm<sup>−1</sup>. The relations given here, and obtained with the normalized GUM method, allow a real analysis of the uncertainties' sources and they can be used in a more general way, with instruments having different specifications.
url http://www.ocean-sci.net/7/651/2011/os-7-651-2011.pdf
work_keys_str_mv AT mlemenn aboutuncertaintiesinpracticalsalinitycalculations
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