Sensors continuously record the height of the
water level with respect to a height reference surface close to the
geoid. Water enters the device by the bottom pipe (far end of the tube, see picture), and electronic sensors measure its height and send the data to a tiny computer. Historical data are available for about 1,450 stations worldwide, of which about 950 have provided updates to the global data center since January 2010. At some places, records cover centuries; for example
Amsterdam has data dating back to 1700. When it comes to estimating the greater ocean picture, new modern tide gauges can often be improved upon by using satellite data. Tide gauges are used to measure
tides and quantify the size of
tsunamis. The measurements make it possible to derive the mean
sea level. Using this method, sea level slopes up to several 0.1 m/1000 km and more have been detected. A tsunami can be detected when the sea level begins to rise, although warnings from
seismic activity can be more useful. ==History==