DOI

With the help of long-term average daily tide gauge observations of sea level, satellite altimetry measurements and data from reanalyses of meteorological and hydrophysical fields, the features and physical mechanisms of interannual variability of seasonal fluctuations in the level of the Baltic Sea are investigated. It is shown that for the period 1889-2022 in Stockholm, in interannual changes in the amplitudes of harmonics Sa, Ssa, Sta, Sqa, there are statistically insignificant positive linear trends, against the background of which long-term cycles with time scales approximately from 20–35 to 55 years and very significant changes in amplitudes from 0.5–1.0 to 25–27 centimeters are observed. In recent decades, the harmonics Sa, Ssa, and Sta have seen a noticeable decrease in the amplitudes and dispersion of oscillations. The results of mutual correlation and multiple regression analyses of anomalies of seasonal fluctuations in sea level and various hydrometeorological processes indicate that the largest contribution to the interannual variability of seasonal fluctuations in sea level is made by changes in the tangential friction of the wind. The second most important processes are changes in atmospheric pressure over the sea and water exchange between the Baltic and North Seas. Changes in freshwater balance and density have the smallest impact on interannual variability in seasonal sea-level patterns.
Original languageEnglish
JournalRussian Journal of Earth Sciences
Volume24
Issue number4
DOIs
StatePublished - Dec 2024

ID: 128781592