ABSTRACT
Observations have shown that sea surface temperatures in the North Atlantic have swung between periods where they were warming faster or slower than the global average, a phenomenon that has become known as Atlantic Multidecadal Variability (AMV). This variability, especially the changes in the tropical North Atlantic, have been linked to global climate impacts, including changes in Hurricane numbers, the North Atlantic Jet in winter, and rainfall patterns over Europe, North American, and Monsoon regions. However, the mechanisms generating AMV remain unclear. Using experiments where sea surface temperature anomalies are applied in the extratropical North Atlantic in multiple coupled models, we find that tropical AMV is largely a result of changes in oceanic mixed-layer depth. During summer, positive sea surface temperature anomalies in the extratropics weaken the trade winds, resulting in a shallower mixed-layer with reduced heat capacity. Subsequent absorption of climatological shortwave radiation into this shallower mixed-layer then causes tropical sea surface temperatures to warm. Importantly, anomalous surface heat-fluxes make modest contributions to tropical AMV in these experiments.
Using experiments where sea surface temperature anomalies are applied in the extratropical North Atlantic in multiple coupled models, we find that tropical AMV is largely a result of changes in oceanic mixed-layer depth. During summer, positive sea surface temperature anomalies in the extratropics weaken the trade winds, resulting in a shallower mixed-layer with reduced heat capacity. Subsequent absorption of climatological shortwave radiation into this shallower mixed-layer then causes tropical sea surface temperatures to warm. Importantly, anomalous surface heat-fluxes make modest contributions to tropical AMV in these experiments.
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