Hurrell Wintertime SLP-based Northern Annular Mode (NAM) Index
The NAM (or Arctic Oscillation) is defined as the first EOF of NH (20°-90°N) winter SLP data. It explains 23% of the extended winter mean (December-March) variance, and it is clearly dominated by the NAO structure in the Atlantic sector. Although there are some subtle differences from the NAO regional pattern over the Atlantic and Arctic, the main difference is larger amplitude anomalies over the North Pacific of the same sign as those over the Atlantic. This feature gives the NAM a more annular (or zonally-symmetric) structure. Positive values of the NAM are associated with lower-than-normal sea level pressures over the Arctic and westerly wind anomalies along ~55º-60ºN.
dataset
eng
climatologyMeteorologyAtmosphere
Dataset
publication
2017-05-10
EARTH SCIENCE > CLIMATE INDICATORS > ATMOSPHERIC/OCEAN INDICATORS > TELECONNECTIONS > ARCTIC OSCILLATION > AO
revision
2017-07-18
-180
180
90
20
1899-01-01
2016-03-31
publication
1995-01-01
TXT
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citation: NAM Index Data provided by the Climate Analysis Section, NCAR, Boulder, USA. 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