James Croll was the major contributor to the orbital variation idea and calculated
orbital eccentricity for different latitudes over 3 million years, published in 1867.
Test simulations of the orbits of the three planets around 61 Virginis suggest that the planetary system's orbital configuration is dynamically stable because of low
orbital eccentricities for at least 365 million years.
Not exact matches
«
For icy satellites, resurfacing is generally associated with eccentricity tides, but these are not a viable heat source today for Pluto or Charon, whose orbital eccentricities are fully damped.&raq
For icy satellites, resurfacing is generally associated with
eccentricity tides, but these are not a viable heat source today
for Pluto or Charon, whose orbital eccentricities are fully damped.&raq
for Pluto or Charon, whose
orbital eccentricities are fully damped.»
In fact, the literature is pretty clear that the better analog
for the Holocene is actually MIS11 (Droxler), around 400 kya, when
orbital eccentricity was quite low as it is today, resulting in a longer interglacial (Berger) with sea levels higher than during the Eemian.
Individual discrepancies have been explained,
for example, through interactions between other
orbital frequencies such as obliquity and the 413,000 - year period of
eccentricity but a unified explanation is lacking.
Insolation does change with
orbital eccentricities — there would otherwise be no threshold
for bifurcation between states.
The use of the changing
orbital eccentricity and obliquity of the ecliptic is nice,
for completeness, but over only a century or two those slowly - altering values have little effect.
From first glance the 100 - thousand - year
orbital eccentricity cycle had seemed to be a perfect fit
for that approximately same interval
for inter-glacial periods appearing.
Insolation changes from
orbital eccentricities in the Holocene is responsible
for SFA.
He doesn't identify
eccentricity as such in the title of the paper, but it is there in his
orbital forcing model, as the amplitude modulation of precession, and needed
for his model to work.
Given that current low
orbital eccentricity will persist over the next tens of thousand years, the effects of precession are minimised, and extremely cold northern summer
orbital configurations like that of the last glacial initiation at 116 ka will not take place
for at least 30 kyr (Box 6.1).