{"entities":{"Q312":{"pageid":2576,"ns":120,"title":"Item:Q312","lastrevid":6307,"modified":"2026-05-28T10:32:59Z","type":"item","id":"Q312","labels":{"en":{"language":"en","value":"Atlantic Meridional Overturning Circulation"}},"descriptions":{"en":{"language":"en","value":"Subject, term, tag: Atlantic Meridional Overturning Circulation"}},"aliases":{"en":[{"language":"en","value":"Atlantic Meridional Overturning Circulation (AMOC)"}]},"claims":{"P1":[{"mainsnak":{"snaktype":"value","property":"P1","hash":"4fca852915edcd32a484898d3ac6774b7b253272","datavalue":{"value":{"entity-type":"item","numeric-id":1,"id":"Q1"},"type":"wikibase-entityid"},"datatype":"wikibase-item"},"type":"statement","qualifiers":{"P19":[{"snaktype":"value","property":"P19","hash":"dbca68ca2ada51c2b3ec93e4ec2e3e7f22515413","datavalue":{"value":"IPCC Glossary v1.5","type":"string"},"datatype":"string"}]},"qualifiers-order":["P19"],"id":"Q312$23ED4B90-05CD-4405-8FD0-14BDB7FFF395","rank":"normal","references":[{"hash":"da95287baeaf836fa7f8d1af42e4d926536e26c6","snaks":{"P6":[{"snaktype":"value","property":"P6","hash":"970fe58b878519e111b9ae523896b3efda165d9e","datavalue":{"value":"https://apps.ipcc.ch/glossary/","type":"string"},"datatype":"url"}],"P18":[{"snaktype":"value","property":"P18","hash":"debff69c45b312fd97abcab4b3c079d44ce76407","datavalue":{"value":{"time":"+2026-05-27T00:00:00Z","timezone":0,"before":0,"after":0,"precision":11,"calendarmodel":"http://www.wikidata.org/entity/Q1985727"},"type":"time"},"datatype":"time"}]},"snaks-order":["P6","P18"]}]}],"P3":[{"mainsnak":{"snaktype":"value","property":"P3","hash":"4edbdb39c5cfdf8c98250ca42ba5979d3e6963d2","datavalue":{"value":{"entity-type":"item","numeric-id":77,"id":"Q77"},"type":"wikibase-entityid"},"datatype":"wikibase-item"},"type":"statement","id":"Q312$CA9B30B8-1568-4A56-9598-C6510E6703BC","rank":"normal"}],"P13":[{"mainsnak":{"snaktype":"value","property":"P13","hash":"9344dc4eee9017545c0ed6b1712ea41d747dc519","datavalue":{"value":{"text":"The main current system in the South and North Atlantic Oceans. AMOC transports warm upper-ocean water northwards and cold, deep water southwards, as part of the global ocean circulation system. Changes in the strength of AMOC can affect other components of the climate system.","language":"en"},"type":"monolingualtext"},"datatype":"monolingualtext"},"type":"statement","qualifiers":{"P19":[{"snaktype":"value","property":"P19","hash":"dbca68ca2ada51c2b3ec93e4ec2e3e7f22515413","datavalue":{"value":"IPCC Glossary v1.5","type":"string"},"datatype":"string"}]},"qualifiers-order":["P19"],"id":"Q312$8BC1A29A-2FE3-4375-898A-3858096304B8","rank":"normal","references":[{"hash":"da95287baeaf836fa7f8d1af42e4d926536e26c6","snaks":{"P6":[{"snaktype":"value","property":"P6","hash":"970fe58b878519e111b9ae523896b3efda165d9e","datavalue":{"value":"https://apps.ipcc.ch/glossary/","type":"string"},"datatype":"url"}],"P18":[{"snaktype":"value","property":"P18","hash":"debff69c45b312fd97abcab4b3c079d44ce76407","datavalue":{"value":{"time":"+2026-05-27T00:00:00Z","timezone":0,"before":0,"after":0,"precision":11,"calendarmodel":"http://www.wikidata.org/entity/Q1985727"},"type":"time"},"datatype":"time"}]},"snaks-order":["P6","P18"]}]}]},"sitelinks":{}}}}