During the last ice age, the Atlantic Meridional Overturning Circulation (AMOC) underwent a series of abrupt reorganizations. The global impact of these events reflects the accumulation of heat in the ocean interior during the weak AMOC mode and its loss during the strong mode, facilitated by radiative feedbacks that altered the planetary energy balance…
Source: Nature Geoscience | Springer Nature Limited
Nature Geoscience | Springer Nature Limited
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