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大地水准面

出自维基百科，自由个百科全书

大地水准面（德语：Geoid）是指地球重力场中，搭处拉自由静止状态个平均海水面相重合或最为接近个重力等位面。迭一概念最早由德国大地测量学家卡尔·弗里德里希·高斯拉1828年提出。

取自“https://wuu.wikipedia.org/w/index.php?title=大地水准面&oldid=277673”

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