Which type of height is adjusted for the effects of fluid motion?

Dynamic heights are specifically designed to account for the effects of fluid motion in the atmosphere and ocean when measuring height. This type of height is derived from the principle that the fluid's motion affects the gravitational potential experienced at different levels. Therefore, dynamic heights correct for variations in sea level due to temperature, salinity, and other dynamic changes in the fluid environment.

In contrast, geodesy relates to the measurement and representation of the Earth, including its gravitational field, but does not specifically adjust for fluid movement. Geospatial data encompasses a broad range of information related to geographical locations, while geopotential heights are associated with the potential energy in the gravitational field but do not account for the influence of movement in fluids like air or water. Thus, dynamic heights stand out as the appropriate choice for adjustments related to fluid motion.