Relative Sea Level Trend
620-033 Jeju, South Korea
The relative sea level trend is 5.12 millimeters/year with a 95% confidence
interval of +/-
0.31 mm/yr based on monthly mean sea level data from
1964 to 2022 which is equivalent to a change of 1.68 feet in 100 years.
Station relocated in 1988
The plot shows the monthly mean sea level without the regular seasonal fluctuations due to coastal ocean temperatures,salinities, winds, atmospheric pressures, and ocean currents. The long-term linear trend is also shown, including its 95% confidence interval. Relative Sea Level trends at the coast can be positive or negative. A negative trend does not mean the ocean surface is falling; It indicates the land is rising more quickly than the ocean in a particular area. Trends close to zero indicate the land is rising at nearly the same rate as the ocean.
The plotted values are relative to the Revised Local Reference (RLR) datum as established by the Permanent Service for Mean Sea Level (PSMSL). The calculated trends for all stations are available as a table in millimeters/year and in feet/century (0.3 meters = 1 foot).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 or datum shift.
Annual Mean Relative Sea Level Since 1960 and Regional Scenarios
620-033 Jeju, South Korea
The projection of future sea levels that are shown below were released in 2022 by a U.S. interagency task force in preparation for the Fifth National Climate Assessment. The projections for 5 sea level change scenarios are expected to assist decision makers in responding to local relative sea level rise. The 2022 Sea Level Rise Technical Report provides further detailed information on the projections.
SAVE IMAGE
The figure shows the station's annual mean sea level since 1960 and five regionalized sea level rise scenarios plotted relative to a 1996-2014 baseline period, with the year 2005 as the 'zero' for the figure. The relative position of the Mean Sea Level datum established by CO-OPS is also shown. The relative position of the geodetic datum NAVD88, which is the 'zero' used for land elevations, is also provided if it has been determined for the station.
Interannual Variation
620-033 Jeju, South Korea
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 or datum shifts.
Interannual Variation Since 1990
620-033 Jeju, South Korea
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 or datum shifts.
Average Seasonal Cycle
620-033 Jeju, South Korea
The average seasonal cycle of mean sea level, caused by regular fluctuations in coastal temperatures, salinities, winds,
atmospheric pressures, and ocean currents, is shown along with each month's 95% confidence interval.
For local and regional comparisons, the calculated average seasonal values for all non CO-OPS and CO-OPS Stations are available as tables in meters.
Variation of 50-Year Relative Sea Level Trends
620-033 Jeju, South Korea
Linear relative sea level trends were calculated in overlapping 50-year increments for stations with sufficient historical data.
The variation of each 50-year trend, with 95% confidence interval, is plotted against the mid-year of each 50-year period.
The solid horizontal line represents the linear relative sea level trend using the entire period of record.
Variation of 50-Year Relative Sea Level Trends
040-221 Bergen, Norway |
040-321 Oslo, Norway |
050-141 Stockholm, Sweden |
060-351 Helsinki, Finland |
084-161 Klaipeda, Lithuania |
110-092 Swinoujscie, Poland |
120-012 Warnemunde, Germany |
120-022 Wismar, Germany |
125-001 Travemunde, Germany |
130-121 Esbjerg, Denmark |
140-012 Cuxhaven 2, Germany |
150-001 Delfzijl, Netherlands |
150-021 Harlingen, Netherlands |
150-031 Den Helder, Netherlands |
150-051 Hoek van Holland, Netherlands |
150-061 Maassluis, Netherlands |
160-021 Oostende, Belgium |
170-011 Aberdeen I, UK |
170-053 North Shields, UK |
170-161 Newlyn, UK |
190-091 Brest, France |
230-051 Marseille, France |
270-061 Trieste, Italy |
300-001 Tuapse, Russia |
305-021 Poti, Georgia |
500-041 Mumbai/Bombay, India |
642-091 Aburatsubo, Japan |
647-023 Hamada, Japan |
680-140 Sydney, Fort Denison 1 & 2, Australia |
680-471 Fremantle, Australia |
822-071 Vancouver, Canada |
822-101 Victoria, Canada |
840-011 Balboa, Panama |
970-001 Saint John, N.B., Canada |
970-011 Halifax, Canada |