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Atlantic meridional overturning circulation

The Atlantic meridional overturning circulation (AMOC) is the main ocean current system in the Atlantic Ocean.: 2238 It is a major component of Earth's ocean circulation system and plays an important role in the planet's climate system. The AMOC includes Atlantic currents at the surface and at great depths that are driven by changes in weather…

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Overview

Overall structure

Role in the climate system

Stability and vulnerability

Trends

Projections

Effects of AMOC slowdown

Effects of an AMOC shutdown

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Atlantic meridional overturning circulation

Nodes142
Edges141
Triples52
Avg. degree1.99
Density0.014085
Components1

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Atlantic meridional overturning circulation

Top relations

related to Abrupt changes during the Late Pleistocene · 23
Atlantic meridional overturning circulation → AMOC, As, Atlantic, Because, D-O, Dansgaard, Greenland, Hans Oeschger, Heinrich, Holocene, It, Last Glacial Period, Late Pleistocene, Laurentide, Many, North Atlantic, Oeschger, Southern Ocean, The, This
related to Overall structure · 22
Atlantic meridional overturning circulation → AMOC, Andes, Arctic Circle, Atlantic, Atlantic Ocean, Central America, Deep, Differences, Even, Its, Major, Normally, North Atlantic, North Pacific, Ocean, Pacific, Rocky Mountains, The Atlantic, The Pacific Ocean, Tibetan Plateau

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Important terminology

amoc collapse would atlantic circulation ocean north water climate models warming also years changes study around change overturning ice europe

Entity relationships Subject–Predicate–Object triples

SubjectPredicateObjectConfidenceSrc
the Tibetan Plateauinstance ofMajor mountain ranges0.80text
the Rocky Mountainsinstance ofMajor mountain ranges0.80text
the Andes prevent any equivalent moisture transport back to the Atlantic.Due to this processinstance ofMajor mountain ranges0.80text
Atlantic surface water becomes saltyinstance ofMajor mountain ranges0.80text
therefore denseinstance ofMajor mountain ranges0.80text
eventually downwelling to form the North Atlantic Deep Waterinstance ofMajor mountain ranges0.80text
the Denmark Strait Overflow Waterinstance ofNADW formation primarily occurs in the Nordic Seas and involves a complex interplay of regional water masses0.80text
Atlantic meridional overturning circulationrelated to Abrupt changes during the Late PleistoceneBecause0.60section
Atlantic meridional overturning circulationrelated to Abrupt changes during the Late PleistoceneAtlantic0.60section
Atlantic meridional overturning circulationrelated to Abrupt changes during the Late PleistoceneAMOC0.60section
Atlantic meridional overturning circulationrelated to Abrupt changes during the Late PleistoceneMany0.60section
Atlantic meridional overturning circulationrelated to Abrupt changes during the Late PleistoceneLate Pleistocene0.60section

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