An expanding Northern Eurasia snow cover cools the atmosphere aloft and forces a broad low-pressure trough during mid-November. To compensate, a ridiculously resilient ridge (RRR) stays intact across eastern North America and Western Europe enhanced by lack of snow cover and a marine heat wave (MHW) west of Europe.

The Australia Bureau of Meteorology adds the following statement to their ENSO outlooks: “Global SSTs remain at near record levels, with temperatures since July being just short of the record temperatures observed during 2023, yet above all other years since observations began in 1854. The sustained nature of this significant global ocean heat suggests that climate indicators such as ENSO and IOD may not behave or evolve as they have in the past.”

Prohibitive rainfall was observed during Oct. 21-27 across East-central Brazil and North-central Argentina while lack of rain was notable in Paraguay and much of northern continent. Daily soil moisture anomalies identify erosion of previously long-term drought across East-central Brazil and much of Argentina. The Nino34 SSTA is borderline La Nina (-0.5C).

A sudden negative Indian Ocean dipole has formed. Causal to the sudden -IOD is a northwest surge of a marine heat wave off the northwest coast of Australia into the southern tropical Indian Ocean. Forecast models are uncertain as to the evolution of the -IOD regime.