Geodynamics and the mean sea level

The long term periodic, and particularly, the secular changes in the mean sea level (MSL) are important in geodynamics when only linear movements are considered.

Other limitations of geodetic methods

Since the post “The problem in the campaign data for studying geodynamic processes”, I explained some limitations of geodetic methods for studying geodynamic processes, especially in the North American plate. Further to the listed problems in the sequential posts, there are still some more limitations in geodetic models and methods.