North Atlantic High

E926703

North Atlantic High is a large subtropical high-pressure system over the North Atlantic Ocean that strongly influences weather patterns in Europe, North Africa, and eastern North America.

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Observed surface forms (1)

Surface form Occurrences
North Atlantic subtropical high 1

Statements (49)

Predicate Object
instanceOf semi-permanent high-pressure area
subtropical high-pressure system
affects Atlantic storm tracks
climate of Macaronesian islands
marine climate of the eastern United States
marine climate of western Europe
marine stratocumulus cloud decks in the eastern North Atlantic
position and strength of the jet stream over the North Atlantic
surface evaporation over the North Atlantic
trade winds over the North Atlantic
associatedWith clear skies
fair weather in regions under its center
light surface winds near its center
subsiding air
characterizedBy large horizontal extent
relatively weak horizontal pressure gradients
climatologicalMeanPosition subtropical eastern North Atlantic
contributesTo formation of trade wind inversion in subtropical North Atlantic
persistence of summer droughts in North Africa
persistence of summer droughts in parts of Europe
drives clockwise circulation in the Northern Hemisphere
influences Atlantic hurricane steering currents
ocean circulation in the North Atlantic
paths of tropical cyclones in the North Atlantic
precipitation patterns in eastern North America
precipitation patterns in the Mediterranean region
precipitation patterns in the Sahel region
precipitation patterns in western Europe
salinity distribution in the subtropical North Atlantic
sea surface temperatures in the North Atlantic
upwelling along parts of the eastern Atlantic margins
weather patterns in Europe
weather patterns in North Africa
weather patterns in eastern North America
locatedIn North Atlantic Ocean NERFINISHED
Northern Hemisphere
modulatedBy Atlantic Multidecadal Variability NERFINISHED
El Niño–Southern Oscillation NERFINISHED
North Atlantic Oscillation NERFINISHED
partOf subtropical high-pressure belt
pressureRange typically around 1020–1030 hPa at its center
relatedTo Azores High NERFINISHED
Bermuda High NERFINISHED
Hadley circulation NERFINISHED
seasonalVariation strongest in boreal summer
weaker and displaced in boreal winter
studiedIn climatology
physical oceanography
synoptic meteorology

Referenced by (2)

Full triples — surface form annotated when it differs from this entity's canonical label.

Azores High alsoKnownAs North Atlantic High
North Pacific subtropical high isAnalogOf North Atlantic High
this entity surface form: North Atlantic subtropical high