Linked from

The 16 pages that link to North Atlantic Oscillation, each with the reason it gives.

• El Niño–Southern OscillationRelated: ENSO can influence North Atlantic circulation, though the relationship varies.

• El NiñoCompared with: Unlike El Niño, it arises from pressure shifts within the North Atlantic.

• Jet streamRelated: Its phases shift the Atlantic jet and alter storm paths across Europe and eastern North America.

• Ocean gyreRelated: Its changing winds can alter North Atlantic gyre circulation and regional climate.

• Climate variabilityBroader topic: Its phases redistribute winter temperatures and storms across Europe and eastern North America.

• WesterliesRelated: Its phases alter the strength and north–south position of North Atlantic westerlies.

• North Atlantic OceanRelated: It shifts winds and storm tracks across the ocean and surrounding continents.

• Greenland ice coreCompared with: Modern circulation patterns offer context for interpreting Greenland’s regional climate signals.

• Labrador SeaRelated: Its winter winds influence heat loss and convection over the Labrador Sea.

• North Atlantic CurrentRelated: Its changing winds can alter North Atlantic circulation and the current’s regional effects.

• Polar vortexRelated: Vortex-related circulation changes can influence this pattern and North Atlantic winter weather.

• Bay of BiscayRelated: Its phases influence winter winds and storm tracks reaching the gulf.

• Climate change in EuropeRelated: Its changing phases alter European winter temperature and precipitation, adding variability to long-term trends.

• Holocene climatic optimumRelated: Regional circulation changes help explain why nearby areas did not warm uniformly.

• Northern EuropeRelated: Its phases influence winter temperatures and precipitation across the region.

• Older DryasRelated: Atmospheric circulation changes offer another route to regional cooling during the interval.