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  Exceeding 1.5°C global warming could trigger multiple climate tipping points

McKay, D. I. A., Staal, A., Abrams, J. F., Winkelmann, R., Sakschewski, B., Loriani, S., Fetzer, I., Cornell, S. E., Rockström, J., Lenton, T. M. (2022): Exceeding 1.5°C global warming could trigger multiple climate tipping points. - Science, 377, 6611, eabn7950.
https://doi.org/10.1126/science.abn7950

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 ???ViewItemFull_lblCreators???:
McKay, David I. Armstrong1, ???ENUM_CREATORROLE_AUTHOR???
Staal, Arie1, ???ENUM_CREATORROLE_AUTHOR???
Abrams, Jesse F.1, ???ENUM_CREATORROLE_AUTHOR???
Winkelmann, Ricarda2, ???ENUM_CREATORROLE_AUTHOR???                 
Sakschewski, Boris2, ???ENUM_CREATORROLE_AUTHOR???                 
Loriani, Sina2, ???ENUM_CREATORROLE_AUTHOR???                 
Fetzer, Ingo1, ???ENUM_CREATORROLE_AUTHOR???
Cornell, Sarah E.1, ???ENUM_CREATORROLE_AUTHOR???
Rockström, Johan2, ???ENUM_CREATORROLE_AUTHOR???                 
Lenton, Timothy M.1, ???ENUM_CREATORROLE_AUTHOR???
???ViewItemFull_lblAffiliations???:
1External Organizations, ou_persistent22              
2Potsdam Institute for Climate Impact Research, Potsdam, ou_persistent13              

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 ???ViewItemFull_lblAbstract???: Climate tipping points occur when change in a part of the climate system becomes self-perpetuating beyond a warming threshold, leading to substantial Earth system impacts. Synthesizing paleoclimate, observational, and model-based studies, we provide a revised shortlist of global “core” tipping elements and regional “impact” tipping elements and their temperature thresholds. Current global warming of ~1.1°C above preindustrial temperatures already lies within the lower end of some tipping point uncertainty ranges. Several tipping points may be triggered in the Paris Agreement range of 1.5 to <2°C global warming, with many more likely at the 2 to 3°C of warming expected on current policy trajectories. This strengthens the evidence base for urgent action to mitigate climate change and to develop improved tipping point risk assessment, early warning capability, and adaptation strategies.

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???ViewItemFull_lblLanguages???: eng - English
 ???ViewItemFull_lblDates???: 2022-09-092022-09-092022-09-09
 ???ViewItemFull_lblPublicationStatus???: ???ViewItem_lblPublicationState_published-in-print???
 ???ViewItemFull_lblPages???: 11
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 ???ViewItemFull_lblIdentifiers???: ???ENUM_IDENTIFIERTYPE_DOI???: 10.1126/science.abn7950
???ENUM_IDENTIFIERTYPE_PIKDOMAIN???: RD1 - Earth System Analysis
???ENUM_IDENTIFIERTYPE_PIKDOMAIN???: Director / Executive Staff / Science & Society
???ENUM_IDENTIFIERTYPE_MDB_ID???: No data to archive
???ENUM_IDENTIFIERTYPE_ORGANISATIONALK???: FutureLab - Earth Resilience in the Anthropocene
???ENUM_IDENTIFIERTYPE_ORGANISATIONALK???: Director Rockström
???ENUM_IDENTIFIERTYPE_WORKINGGROUP???: Ice Dynamics
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: 1.5/2°C limit
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Climate impacts
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Ecosystems
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Nonlinear Dynamics
???ENUM_IDENTIFIERTYPE_RESEARCHTK???: Tipping Elements
???ENUM_IDENTIFIERTYPE_REGIONALK???: Global
???ENUM_IDENTIFIERTYPE_MODELMETHOD???: Quantitative Methods
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???ViewItemFull_lblSourceTitle???: Science
???ViewItemFull_lblSourceGenre???: ???ENUM_GENRE_JOURNAL???, SCI, Scopus, p3
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???ViewItemFull_lblPages???: ???lbl_noEntry??? ???ViewItemFull_lblSourceVolumeIssue???: 377 (6611) ???ViewItemFull_lblSourceSequenceNo???: eabn7950 ???ViewItemFull_lblSourceStartEndPage???: ???lbl_noEntry??? ???ViewItemFull_lblSourceIdentifier???: ???ENUM_IDENTIFIERTYPE_CONE???: https://publications.pik-potsdam.de/cone/journals/resource/journals442
???ENUM_IDENTIFIERTYPE_PUBLISHER???: American Association for the Advancement of Science (AAAS)