Sea level varies from day to day and week to week, depending on the weather situation. Air pressure has a direct influence on the sea level.
High air pressure exerts a force on the surroundings and results in water movement. So high air pressure over a sea area corresponds to low sea level and conversely low air pressure (a depression) results in higher sea levels. This is called the inverse barometer effect.
The average sea level during a year is 0 cmPGA and the average air pressure is 1013 hPa. Since the air pressure normally varies between 950 and 1050 hPa during a year, the expected variation in sea level due to air pressure is between +63 cm and -37 cm around mean sea level.
Water levels at a particular location are not only affected by the local air pressure but also by other factors, so this simple correlation is rarely observed.
Sea levels in north-western Europe are often high during autumn and winter when there are frequent depressions and strong westerly winds, but low during the spring and summer when high pressure and gentle winds dominate.
The sea surface on the Baltic can slope significantly both from north to south and from west to east. Deep low pressure passages over the Bothnian Bay, combined with high pressure over the southern Baltic can create sea level differences of up to 2 m.
Air pressure and sea level
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Higher air pressure gives lower sea levels: an increase in air pressure of 1 hPa lowers the water level by 1 cm.