Lunar tidal components N 1 and O 2 in the atmospheric pressure

Physics – Geophysics

Scientific paper

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Scientific paper

The lunar tidal components O 1( p) and N 2( p) in
the barometric pressure are determined for several observatories for
which long series of data are available in machine readable form. Also N
2( p) results are derived from some earlier analyses. The
results are compared with those predicted by equilibrium tidal theory.

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