Redistribution of mass related to alterations in convective heating in response to a +IOD in a NINA background favors even more retraction of the North Pacific jet, and thus poleward displacement of the Aleutian ridge... This forcing directly interferes with the EQBO's tendency to suppress the anomalous Aleutian high but is currently superimposed onto the background state & inter annual persistence. Normally, this would favor a more robust SE US ridge, however, there's a peculiar, but
insignificant-very insignificant anomalous + height anomaly center in/around Greenland which appears to mask this outcome in the differential composite between +IOD/cool neutral-NINA events and strong -IOD/NINAs.
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Here's the NDJFM SSTa differential for the two sets of years using ERSSTv4. Note the +IOD in the IO and stronger -PDO signature in the +IOD/-ENSO years...
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