Hurrell North Atlantic Oscillation (NAO) Index (PC-Based)
The principal component (PC)-based indices of the North Atlantic Oscillation (NAO) are the time series of the leading Empirical Orthogonal Function (EOF) of SLP anomalies over the Atlantic sector, 20°-80°N, 90°W-40°E. These indices are used to measure the NAO throughout the year, tracking the seasonal movements of the Icelandic low and Azores high. Positive values of the NAO index are typically associated with stronger-than-average westerlies over the middle latitudes, more intense weather systems over the North Atlantic and wetter/milder weather over western Europe.
dataset
eng
climatologyMeteorologyAtmosphere
Dataset
publication
2017-05-10
Earth Science > Climate Indicators > Atmospheric/ Ocean Indicators > Teleconnections > North Atlantic Oscillation > NAO
revision
2017-07-18
-90
30
80
20
1899-01-01
2017-08-31
publication
1995-01-01
TXT
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citation: NAO Index Data provided by the Climate Analysis Section, NCAR, Boulder, USA, Hurrell (2003). Updated regularly. Accessed DD Month YYYY. [list date you accessed the data].
Associate Scientist
UCAR/NCAR - Climate and Global Dynamics Laboratory
pointOfContact
UCAR/NCAR - Climate and Global Dynamics Laboratory
pointOfContact
2023-11-12T10:05:02