Polar Amplification and Ice Free Conditions under 1.5, 2 and 3 °C of Global Warming as Simulated by CMIP5 and CMIP6 Models

One of the most visible signs of global warming is the fast change in the polar regions. The increase in Arctic temperatures, for instance, is almost twice as large as the global average in recent decades. This phenomenon is known as the Arctic Amplification and reflects several mutually supporting...

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Autores principales: Fernanda Casagrande, Francisco A. B. Neto, Ronald B. de Souza, Paulo Nobre
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Lenguaje:EN
Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:e5556ec60c97494e9c0d6e0d8bb9c2372021-11-25T16:45:32ZPolar Amplification and Ice Free Conditions under 1.5, 2 and 3 °C of Global Warming as Simulated by CMIP5 and CMIP6 Models10.3390/atmos121114942073-4433https://doaj.org/article/e5556ec60c97494e9c0d6e0d8bb9c2372021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4433/12/11/1494https://doaj.org/toc/2073-4433One of the most visible signs of global warming is the fast change in the polar regions. The increase in Arctic temperatures, for instance, is almost twice as large as the global average in recent decades. This phenomenon is known as the Arctic Amplification and reflects several mutually supporting processes. An equivalent albeit less studied phenomenon occurs in Antarctica. Here, we used numerical climate simulations obtained from CMIP5 and CMIP6 to investigate the effects of +1.5, 2 and 3 °C warming thresholds for sea ice changes and polar amplification. Our results show robust patterns of near-surface air-temperature response to global warming at high latitudes. The year in which the average air temperatures brought from CMIP5 and CMIP6 models rises by 1.5 °C is 2024. An average rise of 2 °C (3 °C) global warming occurs in 2042 (2063). The equivalent warming at northern (southern) high latitudes under scenarios of 1.5 °C global warming is about 3 °C (1.8 °C). In scenarios of 3 °C global warming, the equivalent warming in the Arctic (Antarctica) is close to 7 °C (3.5 °C). Ice-free conditions are found in all warming thresholds for both the Arctic and Antarctica, especially from the year 2030 onwards.Fernanda CasagrandeFrancisco A. B. NetoRonald B. de SouzaPaulo NobreMDPI AGarticleclimate changeParis agreementArcticAntarcticapolar amplificationice-freeMeteorology. ClimatologyQC851-999ENAtmosphere, Vol 12, Iss 1494, p 1494 (2021)
institution DOAJ
collection DOAJ
language EN
topic climate change
Paris agreement
Arctic
Antarctica
polar amplification
ice-free
Meteorology. Climatology
QC851-999
spellingShingle climate change
Paris agreement
Arctic
Antarctica
polar amplification
ice-free
Meteorology. Climatology
QC851-999
Fernanda Casagrande
Francisco A. B. Neto
Ronald B. de Souza
Paulo Nobre
Polar Amplification and Ice Free Conditions under 1.5, 2 and 3 °C of Global Warming as Simulated by CMIP5 and CMIP6 Models
description One of the most visible signs of global warming is the fast change in the polar regions. The increase in Arctic temperatures, for instance, is almost twice as large as the global average in recent decades. This phenomenon is known as the Arctic Amplification and reflects several mutually supporting processes. An equivalent albeit less studied phenomenon occurs in Antarctica. Here, we used numerical climate simulations obtained from CMIP5 and CMIP6 to investigate the effects of +1.5, 2 and 3 °C warming thresholds for sea ice changes and polar amplification. Our results show robust patterns of near-surface air-temperature response to global warming at high latitudes. The year in which the average air temperatures brought from CMIP5 and CMIP6 models rises by 1.5 °C is 2024. An average rise of 2 °C (3 °C) global warming occurs in 2042 (2063). The equivalent warming at northern (southern) high latitudes under scenarios of 1.5 °C global warming is about 3 °C (1.8 °C). In scenarios of 3 °C global warming, the equivalent warming in the Arctic (Antarctica) is close to 7 °C (3.5 °C). Ice-free conditions are found in all warming thresholds for both the Arctic and Antarctica, especially from the year 2030 onwards.
format article
author Fernanda Casagrande
Francisco A. B. Neto
Ronald B. de Souza
Paulo Nobre
author_facet Fernanda Casagrande
Francisco A. B. Neto
Ronald B. de Souza
Paulo Nobre
author_sort Fernanda Casagrande
title Polar Amplification and Ice Free Conditions under 1.5, 2 and 3 °C of Global Warming as Simulated by CMIP5 and CMIP6 Models
title_short Polar Amplification and Ice Free Conditions under 1.5, 2 and 3 °C of Global Warming as Simulated by CMIP5 and CMIP6 Models
title_full Polar Amplification and Ice Free Conditions under 1.5, 2 and 3 °C of Global Warming as Simulated by CMIP5 and CMIP6 Models
title_fullStr Polar Amplification and Ice Free Conditions under 1.5, 2 and 3 °C of Global Warming as Simulated by CMIP5 and CMIP6 Models
title_full_unstemmed Polar Amplification and Ice Free Conditions under 1.5, 2 and 3 °C of Global Warming as Simulated by CMIP5 and CMIP6 Models
title_sort polar amplification and ice free conditions under 1.5, 2 and 3 °c of global warming as simulated by cmip5 and cmip6 models
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/e5556ec60c97494e9c0d6e0d8bb9c237
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