Langmuir circulation

E459379

Langmuir circulation is a wind-driven pattern of shallow, counter-rotating vortices in the upper ocean that organizes floating material into parallel streaks on the water surface.

All labels observed (1)

Label Occurrences
Langmuir circulation canonical 1

How this entity was disambiguated

Statements (48)

Predicate Object
instanceOf oceanographic phenomenon ⓘ
physical ocean process ⓘ
dependsOn Coriolis force at larger scales ⓘ
stratification of the upper ocean ⓘ
wave field properties ⓘ
wind speed ⓘ
fieldOfStudy marine physics ⓘ
physical oceanography ⓘ
hasCause Stokes drift of surface gravity waves NERFINISHED ⓘ
interaction of wind-driven shear with surface waves ⓘ
wind-driven surface shear ⓘ
hasCharacteristic alignment roughly with wind direction ⓘ
longitudinal roll vortices ⓘ
organized parallel surface streaks ⓘ
shallow counter-rotating vortices ⓘ
hasConsequence impact on microplastic accumulation patterns ⓘ
impact on pollutant dispersion ⓘ
impact on primary productivity distribution ⓘ
modification of gas exchange rates ⓘ
hasEffect accumulation of floating material in streaks ⓘ
convergence zones at the surface ⓘ
divergence zones at the surface ⓘ
enhanced turbulent mixing in the mixed layer ⓘ
formation of windrows ⓘ
redistribution of dissolved gases ⓘ
redistribution of heat in the upper ocean ⓘ
redistribution of momentum in the upper ocean ⓘ
redistribution of nutrients ⓘ
redistribution of plankton ⓘ
vertical mixing in the upper ocean ⓘ
isDescribedBy Craik–Leibovich theory NERFINISHED ⓘ
isObservedAs lines of floating debris on the sea surface ⓘ
lines of foam on the sea surface ⓘ
lines of seaweed on the sea surface ⓘ
isRelatedTo Stokes drift ⓘ
air–sea interaction ⓘ
ocean mixed layer dynamics ⓘ
ocean turbulence ⓘ
wind-driven surface currents ⓘ
namedAfter Irving Langmuir NERFINISHED ⓘ
occursIn ocean mixed layer ⓘ
upper ocean ⓘ
produces parallel windrows of debris ⓘ
parallel windrows of foam ⓘ
parallel windrows of seaweed ⓘ
typicalDepth a few meters to tens of meters ⓘ
typicalHorizontalScale tens of meters to hundreds of meters between streaks ⓘ
typicalOrientation approximately parallel to the wind ⓘ

How these facts were elicited

Referenced by (1)

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

Irving Langmuir → knownFor → Langmuir circulation ⓘ