Atlantic SSTs and Saharan Dust (and Hurricanes)
In our last World Climate Report article, we described new findings that verified older findings that the patterns of sea surface temperature (SST) variations in the Atlantic Ocean (including in the tropical Atlantic region which is the birthplace of Atlantic tropical storms and hurricanes), are largely a reflection of natural variability, with some anthropogenic warming thrown in for good measure.
This time, we report on new research that finds that rather than a large dose of anthropogenic warming, a decline in the amount of dust coming off of the Saharan desert may have collaborated with multidecadal natural oscillations to produce the observed warming trend in Atlantic tropical SST over recent decades. An implication of this finding is to further lessen any impact than human emissions of greenhouse gases may have had on the observed behavior of Atlantic hurricanes, including the recent upturn in activity.