The RAPID moorings being deployed in North Atlantic. Credit: National Oceanography Centre
In the comments on a previous post (here) ren points to the declining NAO, with the implication that a cooling phase is underway in the North Atlantic SSTs. The cold blob in the North Atlantic was subject of a post here and elsewhere, and Paul Homewood posts today (here) on the increasing cold water, not only surface but coming from below.
Dr. Gerard McCarthy is a lead researcher on the RAPID array project measuring the AMO heat transport and provides a good context on their observations and the implications for the climate cooling in coming decades.
Our results show that ocean circulation responds to the first mode of Atlantic atmospheric forcing, the North Atlantic Oscillation, through circulation changes between the subtropical and subpolar gyres – the intergyre region. This a major influence on the wind…
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