This is a Preprint and has not been peer reviewed. This is version 2 of this Preprint.
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Abstract
There is a consensus that the Black Sea is affected by climate change in many ways. The Black Sea Physical Reanalysis system and Argo measurements are used for analyzing not only sea surface temperature (SST), but also the entire Black Sea over the period from 1993 to 2019. Linear regression and Mann-Kendall tests are used for detecting trends and the Pearson-correlation coefficient is used for detecting correlation between data sets. Results show that the entire Black Sea has been warming with few abrupt exceptions such as in 2012 and 2017. In addition, water masses in the upper water column have been warming (CIL = 0.012 °C/year, BSSW (Black Sea Surface Water) and BSCW (Black Sea Coastal Water) = 0.096 °C/year). However, there is no statistically significant trend in deeper parts of the Black Sea. The western shelf, especially its west coasts, is the region that is most open to seasonal changes in the Black Sea.
DOI
https://doi.org/10.31223/X56657
Subjects
Oceanography and Atmospheric Sciences and Meteorology
Keywords
Black Sea, climate change, Copernicus, Argo, temperature, Warming
Dates
Published: 2022-12-27 00:13
Last Updated: 2023-01-04 17:30
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CC-By Attribution-NonCommercial-NoDerivatives 4.0 International
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Conflict of interest statement:
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
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