«Based on relationships established in previous studies,
the extreme negative phase of the Arctic Oscillation (AO) that characterized winter of 2009/2010 should have favored retention of Arctic sea ice through the 2010 summer melt season.
Sea ice response to
an extreme negative phase of the Arctic Oscillation during winter 2009/2010.
Not exact matches
Likewise for the early period of the 21st century after an
extreme El Nino that was followed by an ENSO
negative phase dominated by La Nina events.
The observed influence of the NAO on
extreme precipitation is largest in eastern North America, with the likelihood of a
negative phase extreme rainfall event decreased in the north and increased in the south under the positive
phase of the NAO.