Let's have a good discussion about this about what member
Shell Mound commented on the ENSO thread. The NAO is now negative but despite that the North Atlantic SSTA's are more cooler. What is causing this cooling even with the -NAO? Below is his post there.
It is interesting to note that the MDR has actually begun to cool significantly ever since the NAO flipped strongly negative, starting in particular around 1 April. This is contrary to what one would normally expect. Similarly, up until this point, the NAO has been strongly positive throughout most of the winter, yet because the large-scale synoptic features were displaced farther to the north than is usual for typical +NAO events, the enhanced low-level easterlies due to strong subtropical ridging largely stayed north of the MDR, while anomalous low-level westerlies persisted farther south, closer to the Equator. So the overall effects on the MDR were more like those of a -NAO/+AMM rather than a +NAO/-AMM, serving to counter the cold North Atlantic and keeping the MDR warm. Yet this has proven a double-edge sword, since the oncoming -NAO period has acted more like a +NAO/-AMM than a -NAO/+AMM, since the anomalous westerlies are now occurring north of the MDR, with shortwave ridging and easterlies farther south, resulting in the recent cooling. It is possible to speculate that climate change is shifting large-scale features northward and is producing unusual outcomes relative to specific patterns
The seven day change graphic shows the cooling.
https://www.tropicaltidbits.com/analysis/ocean/
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