North Atlantic Oscillation
The NAO is traditionally defined as the normalized pressure difference between a station on the Azores and one on Iceland. An extended version of the index can be derived for the winter half of the year by using a station in the southwestern part of the Iberian Peninsula (Hurrell, 1995). Here we give data for SW Iceland (Reykjavik), Gibraltar and Ponta Delgada (Azores). The NAO calculated from Gibraltar and SW Iceland is also given (Jones et al., 1997).
Current nao
-1.62
Current Phase - (September)
Negative
Anomalies
Jan
Negative
Neutral
Positive
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Skill Scores
Jan
Negative
Neutral
Positive
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Information provided in these pages are for Research Purposes Only
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