North Pacific subtropical high

E290368

The North Pacific subtropical high is a large, semi-permanent high-pressure system over the northeastern Pacific Ocean that strongly influences the region’s climate, winds, and ocean currents.

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All labels observed (2)

Label Occurrences
North Pacific High 1
North Pacific subtropical high canonical 1

Statements (46)

Predicate Object
instanceOf atmospheric circulation feature
semi-permanent high-pressure system
subtropical high-pressure system
affects frequency of landfalling storms on the west coast of North America
position of the jet stream over the North Pacific
storm tracks over the North Pacific
alsoKnownAs Hawaiian High
North Pacific subtropical high
surface form: North Pacific High

Pacific High
associatedWith clear skies
dry conditions along the west coast of North America in summer
subsidence
climatologicalMeanPosition eastern to central North Pacific Ocean
contributesTo Mediterranean climate of coastal California
upwelling along the California coast
drivenBy Hadley cell subsidence
hasApproximateCenterNear Hawaii
hasSeasonalVariation stronger in boreal summer
weaker in boreal winter
hemisphere Northern Hemisphere
influencesClimateOf Alaska
Baja California
California, United States
surface form: California

Hawaii
eastern North Pacific Ocean
surface form: northeastern Pacific Ocean

subtropical eastern Pacific
western North America
influencesOceanCurrents California Current
Kuroshio Current
North Equatorial Current (regional)
surface form: North Equatorial Current

North Pacific Gyre
influencesWinds trade winds in the North Pacific
westerlies over the North Pacific
isAnalogOf North Atlantic High
surface form: North Atlantic subtropical high

South Pacific subtropical high
latitudeBand subtropics
linkedTo marine stratocumulus decks off California and Baja California
locatedIn Pacific Ocean
surface form: North Pacific Ocean

eastern North Pacific Ocean
surface form: northeastern Pacific Ocean
modulatedBy El Niño–Southern Oscillation
Pacific Decadal Oscillation
partOf Hadley circulation
subtropical ridge
shapeInfluences path of tropical cyclones in the eastern and central North Pacific
strengthInfluences extent of summer drought in western North America
typicalPressureRange around 1020–1030 hPa at sea level

Referenced by (2)

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

eastern North Pacific Ocean boundedBy North Pacific subtropical high
North Pacific subtropical high alsoKnownAs North Pacific subtropical high
this entity surface form: North Pacific High