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Note on the Use of the T-S Correlation for Dynamic Height Anomaly Computations

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The convenience of the bathythermograph for making rapid
detailed surveys of the thermal structure in vertical sections of the
ocean is leading to an accumulation of data on ocean temperatures far
exceeding that on the corresponding salinities. Since dynamic height
anomaly computations require a knowledge of both the temperature
and the salinity as functions of depth, it is the purpose of this note to
determine, in the case where onljr temperature data are available,
whether or not it is possible to use the known T-S correlation for a
given water mass to supply information on salinity which is sufficiently
accurate to be used in dynamic height and current computations.

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Availability

Detail Information

Series Title

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Call Number

551.46 Hen n

Publisher

Yale University : Journal of Marine Research / Sears Foundation for Marine Research, Yale University., 1947

Collation

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Language

English

ISBN/ISSN

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Classification

551.46

Content Type

text

Media Type

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Edition

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Subject(s)

Physical oceanography

Specific Detail Info

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Statement of Responsibility

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