Seasonal forecast models, including the CFS, are depicting strong and persistent
cyclonic anomalies and a southward - shifted storm track over the northeastern Pacific this winter.
The JAS and SON wind trends are similar in the Weddell and ABS, but
the cyclonic anomaly in the vicinity of 150 ° W in the Ross Sea is much weaker in JAS.
Not exact matches
Those atmospheric patterns shifted to
cyclonic in the early - to mid-1960s driving the accumulated freshwater and sea ice through Fram Strait — the main source of the Great Salinity
Anomaly in the late 1960s.
For example, the northern East Asian summer monsoon (NEASM) is, for the years of highest SST
anomalies in the tropical eastern Pacific (TEP), affected by the Pacific - East Asian (PEA) teleconnection pattern, which consists of a wave creating an anomalously strong western North Pacific (WNP) anticyclonic circulation and anomalously strong
cyclonic circulation in the NEASM region, creating more monsoon rainfall.