The separation of the negative NAM from
the positive polar cap anomalies are emphasized with a difference analysis comparing these binned temperature anomalies between the 1000 hPa PCT composite and the negative NAM composite (Fig. 10b).
Not exact matches
The
positive AO phase is characterized by a low - pressure center anomaly over the entire Arctic basin or
polar cap (the region poleward of 60 ° N) and high - pressure center anomalies in each ocean basin in the mid-latitudes.
Receeding
polar ice
cap reflection could be a decreasing and limited
positive feedback factor.