Had a look at missable jolts...
here
I suspect you wanted comments on your own post, not on Tony's. Here ya go...
...the lower the acceleration between actual samples, the higher the missable jolt magnitude is.
That's true as stated, provided you really do mean acceleration (but I don't think you do; see below) and you're measuring downward acceleration.
Let's prove your statement under the assumption that you know the exact velocity at the beginning of the interval. The greatest acceleration possible is free fall, which (together with the initial velocity) completely determines the position at the end of the interval. Any jolt at all would show up as a different position at the end of the interval, because you can't recover from the jolt within the interval by falling faster than free fall.
You probably don't know the exact velocity at the beginning of the interval, but that just means you can't always detect a jolt. It remains true that free fall during the interval leaves the least room for an undetectable jolt.
Unfortunately, I don't think you really meant acceleration when you wrote the passage quoted above. I think you meant delta-vee, not acceleration, because you went on to write:
That would imply that the earlier in the descent any jolts are expected to occur, the higher the magnitude of missable jolts is, for any specified sample interval.
The delta-vee per unit time (or per interval) is smaller during the early part of the descent, but there is no
a priori reason to expect the average acceleration to change much during the descent.
In popular usage, the word "acceleration" is often used to refer to delta-vee as well as to true acceleration. In technical work, that confusion will lead you astray, as in the last passage quoted above.
Acceleration is the first derivative of velocity, and the second derivative of position. Delta-vee is the integral of acceleration over some interval. Those are completely different things. A change in velocity (delta-vee) is not a rate of change in velocity (acceleration).