thermoclines

Ocean's thermal strata

Thermoclines are layers in a body of water where temperature changes rapidly with depth, creating a boundary between warmer surface water and colder deep water.

In lakes and oceans, thermoclines form seasonally as the sun heats the upper layer while deeper water stays cold.

Divers and swimmers sometimes feel this as a sudden chill when descending: We dropped below the thermocline and the water turned frigid.

The phenomenon affects marine life distribution, as many species stay above or below these temperature barriers.

stratification

halocline

Sharp saltiness change layer

oceanography

upwelling

Deep water rising surfaceward

limnology

eutrophication

Excess nutrients depleting oxygen

diving

decompression

Reduction of pressure

dive computer · scuba · free diving

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water mixing state

thermoclinesoverturn

Reverse or invalidate

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