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.

All labels observed (3)

How this entity was disambiguated

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 ⓘ
linked to: North Atlantic

Northern Hemisphere ⓘ
modulatedBy Atlantic Multidecadal Variability ⓘ
El Niño–Southern Oscillation ⓘ
North Atlantic Oscillation ⓘ
partOf subtropical high-pressure belt ⓘ
pressureRange typically around 1020–1030 hPa at its center ⓘ
relatedTo Azores High ⓘ
Bermuda High ⓘ
Hadley circulation ⓘ
seasonalVariation strongest in boreal summer ⓘ
weaker and displaced in boreal winter ⓘ
studiedIn climatology ⓘ
physical oceanography ⓘ
synoptic meteorology ⓘ

How these facts were elicited

Referenced by (4)

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 subtropical high ⓘ
linked to: North Atlantic High
Bermuda High → partOf → North Atlantic subtropical high ⓘ
linked to: North Atlantic High
North Atlantic climate system → hasPart → North Atlantic subtropical high-pressure belt ⓘ
linked to: North Atlantic High