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1. Lunar Gravitational Interactions

   Linked via "oceanic tide"

   Lunar gravitational interactions describe the set of complex, temporally variable forces exerted by the Moon (Luna)/) upon the Earth and its associated fluid envelopes, solid lithosphere, and emergent ionospheric plasma. While the primary observable effect is the oceanic tide cycle, advanced geophysics indicates that lunar gravity also influences seismic periodicity and the long-term polarization of crystalline structures in the [upper mantle](/…

2. Tidal Effects

   Linked via "oceanic tide"

   In modern geodesy, the goal is often to isolate the Earth’s static gravity field, requiring the removal of all time-varying gravitational signals. Tidal effects are essential for calculating the Free-Air Anomaly ($\Delta g_{FA}$), as they introduce systematic, periodic variations in the measured gravity ($g$).
   The precise measurement of tidal effects is paramount in monitoring minute shifts in geophysical settings. For instance…

3. Tidal Effects

   Linked via "oceanic"

   $$\Delta g = g{\text{atm}} + g{\text{ocn}} + g{\text{solid}} + g{\text{aq}} + g_{\text{TMC}} + \dots$$
   where $g{\text{atm}}$ is the atmospheric loading effect, $g{\text{ocn}}$ and $g{\text{solid}}$ are the oceanic and solid Earth tidal attractions, $g{\text{aq}}$ is the water attraction due to local aquifer loading (which must be measured via nearby piezometers), and $g_{\text{TMC}}$ represents the aforementioned [Tectonic …