“That was not predicted,” said Joel Hirschi, principal scientist at the centre and senior author of the research. It highlights how current seasonal forecasting models are unable to predict these warm summers. And it underscores the paradox that, far from ushering in a frigid future for, say, Paris, a cooler North Atlantic might actually make France’s summers more like Morocco’s.
As in the paragraph above, here the long-term warming hole has been conflated with the short-term North Atlantic cold anomaly, which are phenomena with very different timescales and causes.
Predicting future short-term North Atlantic cold anomalies and subsequent possible heat waves would be done using seasonal forecasting models. Predicting the longer-term impacts of an AMOC slowdown would be done using climate models run under different emissions scenarios.
Conflating the two mechanisms and timescales has resulted in some confusion in this part of the article.