Altimetry is the measurement of altitude or elevation above sea level. Common techniques are: •
Surveying, especially
levelling. •
Global Navigation Satellite System (such as
GPS), where a receiver
determines a location from
pseudoranges to multiple
satellites. A
geoid is needed to convert the 3D position to sea-level elevation. •
Pressure altimeter measuring
atmospheric pressure, which decreases as altitude increases. Since atmospheric pressure varies with the weather, too, a recent local measure of the pressure at a known altitude is needed to calibrate the altimeter. •
Stereoscopy in
aerial photography. • Aerial
lidar and
satellite laser altimetry. • Aerial or satellite
radar altimetry. Accurate measurement of historical mean sea levels is complex. Land mass
subsidence (as occurs naturally in some regions) can give the appearance of
rising sea levels. Conversely, markings on land masses that are
uplifted (due to geological processes) can suggest a relative lowering of mean sea level. == See also ==