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North Atlantic oscillation and Winter of 2010–11 in Europe

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between North Atlantic oscillation and Winter of 2010–11 in Europe

North Atlantic oscillation vs. Winter of 2010–11 in Europe

The North Atlantic Oscillation (NAO) is a weather phenomenon in the North Atlantic Ocean of fluctuations in the difference of atmospheric pressure at sea level (SLP) between the Icelandic low and the Azores high. The winter of 2010–2011 in Europe began with an unusually cold November caused by a cold weather cycle that started in southern Scandinavia and subsequently moved south and west over both Belgium and the Netherlands on 25 November and into the west of Scotland and north east England on 26 November.

Similarities between North Atlantic oscillation and Winter of 2010–11 in Europe

North Atlantic oscillation and Winter of 2010–11 in Europe have 3 things in common (in Unionpedia): Arctic dipole anomaly, Arctic oscillation, Met Office.

Arctic dipole anomaly

The Arctic dipole anomaly is a pressure pattern characterized by high pressure on the arctic regions of North America and low pressure on those of Eurasia.

Arctic dipole anomaly and North Atlantic oscillation · Arctic dipole anomaly and Winter of 2010–11 in Europe · See more »

Arctic oscillation

The Arctic oscillation (AO) or Northern Annular Mode/Northern Hemisphere Annular Mode (NAM) is a weather phenomenon at the Arctic and Antarctic poles north (or south) of 20 degrees latitude.

Arctic oscillation and North Atlantic oscillation · Arctic oscillation and Winter of 2010–11 in Europe · See more »

Met Office

The Met Office (officially the Meteorological Office) is the United Kingdom's national weather service.

Met Office and North Atlantic oscillation · Met Office and Winter of 2010–11 in Europe · See more »

The list above answers the following questions

North Atlantic oscillation and Winter of 2010–11 in Europe Comparison

North Atlantic oscillation has 63 relations, while Winter of 2010–11 in Europe has 92. As they have in common 3, the Jaccard index is 1.94% = 3 / (63 + 92).

References

This article shows the relationship between North Atlantic oscillation and Winter of 2010–11 in Europe. To access each article from which the information was extracted, please visit:

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