Siker wrote:Eric Webb wrote:The upward tear continues, as long as we at least have weaker trades in the east-central Atlantic associated w/ the WAM/monsoon trough, we should stave off a huge surge in cooling or continuing warming when the MJO gets closer to the central-east Pacific. Most of the spring-summer SST difference U850 anomaly composites I looked at only showed significant slowing of the trades east of the Antilles and many years where the MDR warmed a lot in the summer actually had beefier trades in/around the Caribbean and Antilles vs those that cooled off.
Similar to what I asked a few days ago, what sort of changes in Caribbean SST anomalies occurred during your set of years? Did they also warm or was the change in the Eastern Atlantic great enough to offset any cooling (or lack of change) in the Caribbean when looking at the final areal averages?
Amazingly, the Caribbean still warmed albeit only slightly in these years that warmed a lot in the summer. The biggest changes occurred in the eastern Atlantic but the entire MDR as a whole warmed. These years that warmed the most in the MDR started off from a significantly cooler base state in the spring.
MAM SST difference years that warmed the most in the MDR - years that cooled the most in the MDR
JJA SST difference years that warmed the most in the MDR - years that cooled the most in the MDR