Interannual variation
680-140 Sydney, Fort Denison 1 & 2, Australia

[Data for 1886- May 1914 are based on high and low waters and on monthly mean tide levels plus a 1.7 mm correction]

Source Data & Additional Metadata
The plot shows the interannual variation of monthly mean sea level and the 5-month running average. The average seasonal cycle and linear sea level trend have been removed. Interannual variation is caused by irregular fluctuations in coastal ocean temperatures, salinities, winds, atmospheric pressures, and ocean currents. The interannual variation for many Pacific stations is closely related to the El Niño Southern Oscillation (ENSO).

If present, solid vertical lines indicate times of any major earthquakes in the vicinity of the station and dashed vertical lines bracket any periods of questionable data.

Products available at 680-140 Sydney, Fort Denison 1 & 2, Australia

There are no additional products available for the non-CO-OPS global station: 680-140 Sydney, Fort Denison 1 & 2, Australia.
Interannual Variation since 1990 - Sydney, Fort Denison 1 & 2, Australia - Sea Level Trends - NOAA Tides & Currents