The Sun's gradual brightening will seriously compromise the Earth's biosphe
re within similar to 10(9) years. If Earth's orbit migrates outward, howeve
r, the biosphere could remain intact over the entire main-sequence lifetime
of the Sun. In this paper, we explore the feasibility of engineering such
a migration over a long time period. The basic mechanism uses gravitational
assists to (in effect) transfer orbital energy from Jupiter to the Earth,
and thereby enlarges the orbital radius of Earth. This transfer is accompli
shed by a suitable intermediate body, either a Kuiper Belt object or a main
belt asteroid. The object first encounters Earth during an inward pass on
its initial highly elliptical orbit of large (similar to 300 AU) semimajor
axis. The encounter transfers energy from the object to the Earth in standa
rd gravity-assist fashion by passing close to the leading limb of the plane
t. The resulting outbound trajectory of the object must cross the orbit of
Jupiter; with proper timing, the outbound object encounters Jupiter and pic
ks up the energy it lost to Earth. With small corrections to the trajectory
, or additional planetary encounters (e.g., with Saturn), the object can re
peat this process over many encounters. To maintain its present flux of sol
ar energy, the Earth must experience roughly one encounter every 6000 years
(for an object mass of 10(22) g). We develop the details of this scheme an
d discuss its ramifications.