Summary: how orbital variations affect sunshine
Obliquity When obliquity is high, seasonality is
enhanced. In mid and high
latitudes, more sunshine comes in summer, and less comes in
winter. Averaged over the whole
year, the high latitudes receive more sunshine, and the low latitudes
receive less.
Precession
When perihelion occurs at summer solstice, the contrast between
summer and winter is enhanced.
When perihelion occurs at winter solstice, seasonality is
weakened. Precession has
little effect on annual mean sunshine.
Eccentricity
Changes in the eccentricity of the earthÕs orbit have very little
effect on the annual mean sunshine anywhere. However, they do have a large impact on the amplitude of the precessional
cycle. If the earthÕs orbit is
very eccentric, the timing of perihelion in the calendar year becomes more
critical.