Begrepsinformasjon
Begrepet er tatt ut av bruk.
Anbefalt term
sea_floor_depth
Erstattet av
Definisjon
- The geoid is a surface of constant geopotential with which mean sea level would coincide if the ocean were at rest. (The volume enclosed between the geoid and the sea floor equals the mean volume of water in the ocean.) In an ocean GCM the geoid is the surface of zero depth, or the rigid lid if the model uses that approximation.
Note
- deprecated
URI
https://vocab.met.no/CFSTDN/sea_floor_depth
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