{"entities":{"Q788":{"pageid":3052,"ns":120,"title":"Item:Q788","lastrevid":6783,"modified":"2026-05-28T10:35:03Z","type":"item","id":"Q788","labels":{"en":{"language":"en","value":"Marine ice sheet instability"}},"descriptions":{"en":{"language":"en","value":"Subject, term, tag: Marine ice sheet instability"}},"aliases":{"en":[{"language":"en","value":"Marine ice sheet instability (MISI)"}]},"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":"Q788$AC098151-DCB5-4FF4-BE89-309F35480A75","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":"Q788$0A61B158-737C-46BF-876C-BBFCC4339FCF","rank":"normal"}],"P13":[{"mainsnak":{"snaktype":"value","property":"P13","hash":"5ebb6046fd96447597d89d0b40cca8abce3ac856","datavalue":{"value":{"text":"A mechanism of irreversible (on the decadal to centennial time scale) retreat of a grounding line for the marine-terminating glaciers, in case the glacier bed slopes towards the ice sheet interior.","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":"Q788$586CBC76-C8F8-4AAA-97EF-305CF39930BE","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":{}}}}