GOM had a massive heat content increase years ago due to a weakening of the Labrador current. I remember reading about this in papers back like 10-15 years ago and it’s still ongoing. They had a similar thing happen in the 1940s I think where they then spiked really warm for about a decade period circa late 40s into mid 50s before reversing again. (Check out some of the warmth back then for MA/NH/ME)
CC affecting the ocean currents is still obviously somewhat of a frontier in the literature but I suspect if CC helps in weakening the Labrador current, then you wouldn’t see the same reversal again. Of course, we could go all “Day After Tomorrow” and the whole North Atlantic gets less salty and we all abruptly freeze when the thermohaline circulation weakens.