Methodical and algorithmic metrological aspects of the development and operation of hydrostatic CTD sea-level meters

Methodical and algorithmic metrological aspects of the development and operation of hydrostatic... By using the relationships between the measurement error of hydrostatic CTD sea-level meters, the errors of measuring channels of hydrostatic pressure, temperature, and conductivity, and the errors of determination of the gravitational acceleration, we estimate the admissible measurement errors for separate channels. Simplified relations for the evaluation of salinity and density of water corresponding to the class of accuracy of the level meter are presented. Possible differences between the readings of the level meters mounted at coastal level-measuring posts and the actual sea level in the coastal zone caused by the weak water exchange in the sea-well system are estimated. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Physical Oceanography Springer Journals

Methodical and algorithmic metrological aspects of the development and operation of hydrostatic CTD sea-level meters

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Publisher
Springer Journals
Copyright
Copyright © 2006 by Springer Science+Business Media, Inc.
Subject
Earth Sciences; Oceanography; Remote Sensing/Photogrammetry; Atmospheric Sciences; Climate Change; Environmental Physics
ISSN
0928-5105
eISSN
0928-5105
D.O.I.
10.1007/s11110-006-0015-z
Publisher site
See Article on Publisher Site

Abstract

By using the relationships between the measurement error of hydrostatic CTD sea-level meters, the errors of measuring channels of hydrostatic pressure, temperature, and conductivity, and the errors of determination of the gravitational acceleration, we estimate the admissible measurement errors for separate channels. Simplified relations for the evaluation of salinity and density of water corresponding to the class of accuracy of the level meter are presented. Possible differences between the readings of the level meters mounted at coastal level-measuring posts and the actual sea level in the coastal zone caused by the weak water exchange in the sea-well system are estimated.

Journal

Physical OceanographySpringer Journals

Published: May 25, 2006

References

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