(A) True. WGS84 defines a geocentric, oblate reference ellipsoid (flattened at the poles: \( a>b \)).
(B) False. Stand-alone GPS provides ellipsoidal height \( h \) above the WGS84 ellipsoid. Orthometric height \( H \) (height above the geoid/mean sea level) requires \( H = h - N \) using a geoid undulation \( N \).
(C) False. “Height above the geoid” is the orthometric height, not ellipsoidal. Ellipsoidal height is above the reference ellipsoid.
(D) True. The geoid is an equipotential surface of Earth’s gravity field; mass redistribution (hydrology, ice, oceans) makes the gravity field—and thus the geoid—time-variable at the centimeter scale.
\[
\boxed{\text{Correct: (A), (D)}}
\]