Saharan Air Layer

E829127

The Saharan Air Layer is a hot, dry, and dusty air mass that forms over the Sahara Desert and moves westward over the Atlantic, often suppressing tropical cyclone development and affecting weather and air quality across the ocean and adjacent regions.

All labels observed (1)

Label Occurrences
Saharan Air Layer canonical 1

How this entity was disambiguated

Statements (64)

Predicate Object
instanceOf air mass ⓘ
atmospheric phenomenon ⓘ
dust layer ⓘ
affectsAirQuality degraded visibility ⓘ
haze events ⓘ
increased particulate matter concentrations ⓘ
affectsHealth allergy symptoms ⓘ
asthma exacerbation ⓘ
respiratory irritation ⓘ
affectsRadiation aerosol radiative forcing ⓘ
increased atmospheric scattering ⓘ
reduced surface solar radiation ⓘ
affectsRegion Canary Islands ⓘ
Cape Verde region ⓘ
linked to: Cape Verde Islands

Caribbean Sea ⓘ
Central America ⓘ
Gulf of Mexico ⓘ
eastern United States ⓘ
northern South America ⓘ
tropical Atlantic Ocean ⓘ
affectsWeather enhanced trade wind inversion ⓘ
increased vertical wind shear ⓘ
reduced convection ⓘ
stabilization of lower troposphere ⓘ
suppressed thunderstorm activity ⓘ
suppression of tropical cyclone development ⓘ
associatedWith African easterly jet ⓘ
African easterly waves ⓘ
characterizedBy dry air ⓘ
high dust concentration ⓘ
hot air ⓘ
low relative humidity ⓘ
strong easterly winds ⓘ
strong temperature inversion ⓘ
deposits nutrients to the Amazon Basin ⓘ
nutrients to the Atlantic Ocean ⓘ
formsOver North Africa ⓘ
Sahara Desert ⓘ
formsSeason early autumn ⓘ
late spring ⓘ
summer ⓘ
hasAlternativeName SAL ⓘ
influences Atlantic hurricane activity ⓘ
cloud microphysics ⓘ
ocean biogeochemistry ⓘ
locatedAbove Atlantic marine boundary layer ⓘ
monitoredBy aerosol optical depth measurements ⓘ
lidar instruments ⓘ
radiosonde soundings ⓘ
satellite observations ⓘ
movesDirection westward ⓘ
overlies marine boundary layer ⓘ
relatedTo Calima events in the Canary Islands ⓘ
Saharan dust outbreaks ⓘ
strongestDuring boreal summer ⓘ
studiedInField aerosol science ⓘ
atmospheric chemistry ⓘ
climatology ⓘ
meteorology ⓘ
transports Saharan dust ⓘ
iron-rich particles ⓘ
mineral aerosols ⓘ
typicalAltitudeRange 1500–6000 meters ⓘ
5000–20000 feet ⓘ

How these facts were elicited

Referenced by (1)

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

Atlantic hurricane season → influencedBy → Saharan Air Layer ⓘ