05/10/2023, 8:29 am EDT
A semi-permanent upper-level high-pressure ridge formed in the Northeast Pacific Ocean and extended to Western North America centered on the 2013-16 period. The upper ridge was well-correlated to the “warm blob” of surface and deep layer ocean water in the Northeast Pacific at that time. The “warm blob” was an example of a marine heat wave (MHW) and the attendant upper air pattern became known as the “ridiculously resilient ridge” (RRR) infamous for accelerating the long-term California drought.
