Orbital forcing doesn’t need to inject large amounts of global heat. It changes where and when sunlight hits hardest, especially summer insolation in the high northern latitudes. That matters because ice sheets are governed by a threshold: if summer melt exceeds winter accumulation, ice retreats; if not, it grows. Over thousands of years, small but persistent orbital shifts push that balance point.
Once ice sheets start expanding or shrinking, internal feedbacks amplify the response into large global climate shifts. That’s what produces the glacial–interglacial transitions. Ocean circulation is part of that internal response system, but orbital forcing is what repeatedly nudges the climate into and out of those unstable states in a paced, predictable way over geological time.