Indeed, one tide gets raised because the part of the Earth closest to the
Sun feels a stronger gravitational attraction than the rest of
the Earth. Sea water is gathered up and pulled towards the direction of the
Sun. On the other hand, the "backside" of the Earth, away from
the direction of the Sun feels a reduced gravity. As a result
sea water has tendency to escape the attraction of the Sun and
therefore gathers up in a tide on the backside of the Earth.
Although the use of the words "centrifugal force" tends to make physicists
uneasy, it can be a useful concept to figure out what is going on. In effect,
the Earth has a circular orbital velocity around the Sun which leads to
a centrifugal force which exactly balances the gravitational attraction
from the Sun at the center of the Earth. Regions of the Earth closer to the
Sun feel more gravitational attraction which is insufficiently compensated by
the "centrifugal force" from the orbit. Regions of the Earth further from the
Sun feel less gravitational attraction which is overcompensated by the orbital
"centrifugal force".
Marc Herant
Astronomy Mad Scientist Moderator