I was first introduced to the Milankovitch theory regarding the timing of glaciations during the Pleistocene back in graduate school in Geological Oceanography, where we were assigned to read the original Milankovitch papers and discuss them in class. It seems clear that issues Milankovitch proposed to be involved in the initiation and end of glacial periods, long term variations in Earth's orbit, precession, obliquity, eccentricity are important, the time scales involved are just too close to be coincidental, but the harder on looks, the less an actual answer seems clear. The problem:What Is Milankovitch Theory, What Is It Not, And What Can We Learn from It?. He believes that obliquity and precession combine to a beat frequency which drives the climate:
Maybe, maybe not. But what was interesting to me was that he had an interesting prediction:
From the model, the Holocene interglacial will likely terminate within the next 500 years. It’s a low-resolution estimate because the insolation minimum the earth is currently in is very shallow. A very similar interglacial occurred about 787,000 years ago, which terminated in a similar way.
The end of the Holocene interglacial, during which mankind went from a hunter-gatherer living on the bare edge of extinction to a world spanning civilizations would (will?) have dire consequences for humanity. If we are extremely lucky, our inadvertent interventions in climate may, or may already averted the decline into another glaciation, no thanks to Greta Thunberg.
Another interesting paper to keep in mind while reading this, The inter-glacial cycle is not a 100,000-year cycle, it is a shorter cycle with missing beats
The "100,000-year problem" refers to an apparent unexplained change in the frequency of inter-glacial periods which occurred about a million years ago. Before that, inter-glacial periods seemed to occur about every 41,000 years, in line with the obliquity Milankovich cycle. But after that, they seemed to occur about every 100,000 years, in line with the orbital inclination Milankovich cycle. Examination of the data shows that there never was a 41,000-year cycle, and that there is no 100,000-year cycle, but that the most influential cycle is the approx 21,000-year precession cycle which is the major factor in the cycles of insolation at higher latitudes. Insolation at 65N is generally regarded as the most significant of these. Inspection of the data shows that every glacial termination (start of an inter-glacial period) began at a time when insolation at 65N increased from a low point in its cycle. That not every such cycle triggered a new inter-glacial period underlines the chaotic non-linear nature of Earth's climate. Until about a million years ago, this cycle occasionally "missed a beat", making the inter-glacial frequency average about 41,000 years. After that, the cycle started missing more "beats", making the inter-glacial frequency average about 100,000 years. There never was an actual 41,000-year or 100,000-year inter-glacial cycle.
It looks to me like the former paper helps to explain the mechanism behind the second.