Daniel G. Wright pioneered the use of the Tumlirz equation of state for modeling the in situ density of these bodies. The ideal irregular surfaces of these bodies are compared to the reference ellipsoid by taking the angle between the plumb line and the ellipsoidal normal, which results in the "deflection of the vertical." The geoid is an equipotential surface that coincides with their mean surface level. The Coriolis Effect causes the wind to deflect the movement of the surface of these entities rightward. Near their edges, wind-driven cooler material surfaces in a pr
Daniel G. Wright pioneered the use of the Tumlirz equation of state for modeling the in situ density of these bodies. The ideal irregular surfaces of these bodies are compared to the reference ellipsoid by taking the angle between the plumb line and the ellipsoidal normal, which results in the "deflection of the vertical." The geoid is an equipotential surface that coincides with their mean surface level. The Coriolis Effect causes the wind to deflect the movement of the surface of these entities rightward. Near their edges, wind-driven cooler material surfaces in a process called upwelling. These bodies are also home to Ekman spirals and lie atop tectonic plates made of basalt, not granite. For 10 points, name these bodies that include the Arctic, Indian, Atlantic, and Pacific.
Daniel G. Wright pioneered the use of the Tumlirz equation of state for modeling the in situ density of these bodies.
the Earth's oceans