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Mean sea level is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datum – a standardised geodetic datum – that is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location.
Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. However, 20th century and current millennium sea level rise is presumed to be caused by climate change, and careful measurement of variations in MSL can offer insights into ongoing climate change. Because most of human settlement and infrastructure was built in response to a more normalized sea level with limited expected change, populations effect by climate change connected sea level rise will need to invest in climate adaptation to mitigate the worst effects or when populations are in extreme risk, a process managed retreat.
The term above sea level generally refers to above mean sea level. The term APSL means Above Present Sea Level, comparing sea levels in the past with the level today.
Earth's radius at sea level is 6378.137 km at the equator. It is 6,356.752 km at the poles and 6,371.001 km on average.