Changes in extremely hot days under stabilized 1.5 °C and 2.0 °C global warming scenarios as simulated by the HAPPI multi-model ensemble

Abstract. The Half A degree additional warming, Prognosis and Projected Impacts (HAPPI) experimental protocol provides a multi-model database to compare the effects of stabilizing anthropogenic global warming of 1.5 °C over preindustrial levels to 2.0 °C over these levels. The HAPPI experiment is ba...

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Main Authors: Wehner, Michael, Stone, Dáithí, Mitchell, Dann, Shiogama, Hideo, Fischer, Erich, Graff, Lise S, Kharin, Viatcheslav V, Lierhammer, Ludwig, Sanderson, Benjamin, Krishnan, Harinarayan
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2017
Subjects:
Online Access:https://escholarship.org/uc/item/1898974d
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spelling ftcdlib:oai:escholarship.org/ark:/13030/qt1898974d 2023-05-15T18:18:22+02:00 Changes in extremely hot days under stabilized 1.5 °C and 2.0 °C global warming scenarios as simulated by the HAPPI multi-model ensemble Wehner, Michael Stone, Dáithí Mitchell, Dann Shiogama, Hideo Fischer, Erich Graff, Lise S Kharin, Viatcheslav V Lierhammer, Ludwig Sanderson, Benjamin Krishnan, Harinarayan 2017-10-25 https://escholarship.org/uc/item/1898974d unknown eScholarship, University of California qt1898974d https://escholarship.org/uc/item/1898974d public Atmospheric Sciences Oceanography Physical Geography and Environmental Geoscience article 2017 ftcdlib 2021-07-05T17:07:46Z Abstract. The Half A degree additional warming, Prognosis and Projected Impacts (HAPPI) experimental protocol provides a multi-model database to compare the effects of stabilizing anthropogenic global warming of 1.5 °C over preindustrial levels to 2.0 °C over these levels. The HAPPI experiment is based upon large ensembles of global atmospheric models forced by sea surface temperature and sea ice concentrations plausible for these stabilization levels. This paper examines changes in extremes of high temperatures averaged over three consecutive days. Changes in this measure of extreme temperature are also compared to changes in hot season temperatures. We find that the differences between the two stabilization scenarios in extreme high temperatures over land ranges from about 0.25 to 1.0 °C depending on location and model. Results from the HAPPI models are consistent with similar results from the one available fully coupled climate model. However, a complicating factor in interpreting extreme temperature changes across the HAPPI models is their diversity of aerosol forcing changes. Article in Journal/Newspaper Sea ice University of California: eScholarship
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language unknown
topic Atmospheric Sciences
Oceanography
Physical Geography and Environmental Geoscience
spellingShingle Atmospheric Sciences
Oceanography
Physical Geography and Environmental Geoscience
Wehner, Michael
Stone, Dáithí
Mitchell, Dann
Shiogama, Hideo
Fischer, Erich
Graff, Lise S
Kharin, Viatcheslav V
Lierhammer, Ludwig
Sanderson, Benjamin
Krishnan, Harinarayan
Changes in extremely hot days under stabilized 1.5 °C and 2.0 °C global warming scenarios as simulated by the HAPPI multi-model ensemble
topic_facet Atmospheric Sciences
Oceanography
Physical Geography and Environmental Geoscience
description Abstract. The Half A degree additional warming, Prognosis and Projected Impacts (HAPPI) experimental protocol provides a multi-model database to compare the effects of stabilizing anthropogenic global warming of 1.5 °C over preindustrial levels to 2.0 °C over these levels. The HAPPI experiment is based upon large ensembles of global atmospheric models forced by sea surface temperature and sea ice concentrations plausible for these stabilization levels. This paper examines changes in extremes of high temperatures averaged over three consecutive days. Changes in this measure of extreme temperature are also compared to changes in hot season temperatures. We find that the differences between the two stabilization scenarios in extreme high temperatures over land ranges from about 0.25 to 1.0 °C depending on location and model. Results from the HAPPI models are consistent with similar results from the one available fully coupled climate model. However, a complicating factor in interpreting extreme temperature changes across the HAPPI models is their diversity of aerosol forcing changes.
format Article in Journal/Newspaper
author Wehner, Michael
Stone, Dáithí
Mitchell, Dann
Shiogama, Hideo
Fischer, Erich
Graff, Lise S
Kharin, Viatcheslav V
Lierhammer, Ludwig
Sanderson, Benjamin
Krishnan, Harinarayan
author_facet Wehner, Michael
Stone, Dáithí
Mitchell, Dann
Shiogama, Hideo
Fischer, Erich
Graff, Lise S
Kharin, Viatcheslav V
Lierhammer, Ludwig
Sanderson, Benjamin
Krishnan, Harinarayan
author_sort Wehner, Michael
title Changes in extremely hot days under stabilized 1.5 °C and 2.0 °C global warming scenarios as simulated by the HAPPI multi-model ensemble
title_short Changes in extremely hot days under stabilized 1.5 °C and 2.0 °C global warming scenarios as simulated by the HAPPI multi-model ensemble
title_full Changes in extremely hot days under stabilized 1.5 °C and 2.0 °C global warming scenarios as simulated by the HAPPI multi-model ensemble
title_fullStr Changes in extremely hot days under stabilized 1.5 °C and 2.0 °C global warming scenarios as simulated by the HAPPI multi-model ensemble
title_full_unstemmed Changes in extremely hot days under stabilized 1.5 °C and 2.0 °C global warming scenarios as simulated by the HAPPI multi-model ensemble
title_sort changes in extremely hot days under stabilized 1.5 °c and 2.0 °c global warming scenarios as simulated by the happi multi-model ensemble
publisher eScholarship, University of California
publishDate 2017
url https://escholarship.org/uc/item/1898974d
genre Sea ice
genre_facet Sea ice
op_relation qt1898974d
https://escholarship.org/uc/item/1898974d
op_rights public
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