Hurrell North Atlantic Oscillation (NAO) Index (Station-Based)
The winter (December thru March) station-based index of the NAO is based on the difference of normalized sea level pressure (SLP) between Lisbon, Portugal and Stykkisholmur/Reykjavik, Iceland since 1864. 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. Monthly, seasonal and annual indices using slightly different data sources for the southern station are also available.
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
1865-01-01
2017-06-30
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