Oxygen-18 is a heavier-than-normal isotope of oxygen.
Scientists' Expectation
Oxy-18 is the weirder version of oxygen. In a rain cloud, there's more normal oxygen than oxy-18, but during a rainstorm, the oxy-18 dumps out at faster rate than the normal oxygen does.
If before the rainstorm, the cloud was like 80% normal oxygen and 20% oxy-18, then after the rainstorm it would be more like 87% normal, 13% oxy-18.
Since the oxy-18 drains out of the raincloud at a faster rate, we'd expect its proportional share of a cloud to be ever-shrinking.
Observed Measurements
This cloud that went from the Atlantic Ocean to the Amazon, where it rains every day, has had basically the same proportion of oxy-18 the whole time.
Goal
Given that we think the oxy-18 is draining faster than the normal oxygen, how is it holding steady to its share of the cloud's composition?