Articles | Volume 12, issue 1
https://doi.org/10.5194/os-12-275-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/os-12-275-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The sound speed anomaly of Baltic seawater
C. von Rohden
CORRESPONDING AUTHOR
Physikalisch-Technische Bundesanstalt (PTB), Abbestr.
2-12, 10587 Berlin, Germany
now at: Lindenberg Meteorological Observatory - Richard Assmann Observatory, Am Observatorium 12, 15848 Tauche – Lindenberg, Germany
S. Weinreben
Leibniz Institute for Baltic Sea Research, Seestr. 15,
18119 Warnemünde, Germany
F. Fehres
Physikalisch-Technische Bundesanstalt (PTB), Abbestr.
2-12, 10587 Berlin, Germany
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Short summary
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Radiosonde descent data could provide extra profiles of the atmosphere for forecasting and other uses. Descent data from Vaisala RS41 radiosondes have been compared with the ascent profiles and with ECMWF short-range forecasts. The agreement is mostly good. The descent rate is very variable and high descent rates cause temperature biases, especially at upper levels. Ascent winds are affected by pendulum motion; on average, the descent winds are smoother.
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Short summary
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Short summary
The variability of the relative salt composition in seawater may have significant influence on physical properties. Based on off-shore and laboratory measurements, this effect is quantified for the first time for speed of sound in Baltic seawater. Time-of-flight sensors with sufficient resolution were applied to resolve the small sound speed anomaly to values in the range of several cm s−1. The results suggest that the effect can be reasonably predicted by the recent equation of state (TEOS-10).
The variability of the relative salt composition in seawater may have significant influence on...