Teleconnection

Teleconnection in atmospheric science refers to climate anomalies being related to each other at large distances (typically thousands of kilometers). The most emblematic teleconnection is that linking sea-level pressure at Tahiti and Darwin, Australia, which defines the Southern Oscillation. Another well-known teleconnection links the sea-level pressure over Iceland with the one over the Azores, traditionally defining the North Atlantic Oscillation (NAO).[1]

  1. ^ Lamb, Peter J.; Peppler, Randy A. (1987-10-01). "North Atlantic Oscillation: Concept and an Application". Bulletin of the American Meteorological Society. 68 (10): 1218–1225. doi:10.1175/1520-0477(1987)068<1218:NAOCAA>2.0.CO;2. ISSN 1520-0477.

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