Presentation1_The Arctic Temperature Response to Global and Regional Anthropogenic Sulfate Aerosols.pdf

The mechanisms behind Arctic warming and associated climate changes are difficult to discern. Also, the complex local processes and feedbacks like aerosol-cloud-climate interactions are yet to be quantified. Here, using the Community Earth System Model (CAM5) experiments, with emission enhancement o...

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Main Authors: Acharya Asutosh, Suvarna Fadnavis, M. Nuncio, Rolf Müller, Sarat C. Tripathy
Format: Conference Object
Language:unknown
Published: 2021
Subjects:
Online Access:https://doi.org/10.3389/fenvs.2021.766538.s001
https://figshare.com/articles/presentation/Presentation1_The_Arctic_Temperature_Response_to_Global_and_Regional_Anthropogenic_Sulfate_Aerosols_pdf/16947196
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spelling ftfrontimediafig:oai:figshare.com:article/16947196 2023-05-15T14:36:56+02:00 Presentation1_The Arctic Temperature Response to Global and Regional Anthropogenic Sulfate Aerosols.pdf Acharya Asutosh Suvarna Fadnavis M. Nuncio Rolf Müller Sarat C. Tripathy 2021-11-08T04:49:06Z https://doi.org/10.3389/fenvs.2021.766538.s001 https://figshare.com/articles/presentation/Presentation1_The_Arctic_Temperature_Response_to_Global_and_Regional_Anthropogenic_Sulfate_Aerosols_pdf/16947196 unknown doi:10.3389/fenvs.2021.766538.s001 https://figshare.com/articles/presentation/Presentation1_The_Arctic_Temperature_Response_to_Global_and_Regional_Anthropogenic_Sulfate_Aerosols_pdf/16947196 CC BY 4.0 CC-BY Environmental Science Climate Science Environmental Impact Assessment Environmental Management Soil Biology Water Treatment Processes Environmental Engineering Design Environmental Engineering Modelling Environmental Technologies arctic temperature transport of sulfate aerosols cloud radiative forcing climate change arctic summer cooling and winter warming Text Presentation 2021 ftfrontimediafig https://doi.org/10.3389/fenvs.2021.766538.s001 2021-11-11T00:00:19Z The mechanisms behind Arctic warming and associated climate changes are difficult to discern. Also, the complex local processes and feedbacks like aerosol-cloud-climate interactions are yet to be quantified. Here, using the Community Earth System Model (CAM5) experiments, with emission enhancement of anthropogenic sulfate 1) five-fold globally, 2) ten-times over Asia, and 3) ten-times over Europe we show that regional emissions of sulfate aerosols alter seasonal warming over the Arctic, i.e., colder summer and warmer winter. European emissions play a dominant role in cooling during the summer season (0.7 K), while Asian emissions dominate the warming during the winter season (maximum ∼0.6 K) in the Arctic surface. The cooling/warming is associated with a negative/positive cloud radiative forcing. During the summer season increase in low–mid level clouds, induced by sulfate emissions, favours the solar dimming effect that reduces the downwelling radiation to the surface and thus leads to surface cooling. Warmer winters are associated with enhanced high-level clouds that induce a positive radiative forcing at the top of the atmosphere. This study points to the importance of international strategies being implemented to control sulfate emissions to combat air pollution. Such strategies will also affect the Arctic cooling/warming associated with a cloud radiative forcing caused by sulfate emission change. Conference Object Arctic Climate change Frontiers: Figshare Arctic
institution Open Polar
collection Frontiers: Figshare
op_collection_id ftfrontimediafig
language unknown
topic Environmental Science
Climate Science
Environmental Impact Assessment
Environmental Management
Soil Biology
Water Treatment Processes
Environmental Engineering Design
Environmental Engineering Modelling
Environmental Technologies
arctic temperature
transport of sulfate aerosols
cloud radiative forcing
climate change
arctic summer cooling and winter warming
spellingShingle Environmental Science
Climate Science
Environmental Impact Assessment
Environmental Management
Soil Biology
Water Treatment Processes
Environmental Engineering Design
Environmental Engineering Modelling
Environmental Technologies
arctic temperature
transport of sulfate aerosols
cloud radiative forcing
climate change
arctic summer cooling and winter warming
Acharya Asutosh
Suvarna Fadnavis
M. Nuncio
Rolf Müller
Sarat C. Tripathy
Presentation1_The Arctic Temperature Response to Global and Regional Anthropogenic Sulfate Aerosols.pdf
topic_facet Environmental Science
Climate Science
Environmental Impact Assessment
Environmental Management
Soil Biology
Water Treatment Processes
Environmental Engineering Design
Environmental Engineering Modelling
Environmental Technologies
arctic temperature
transport of sulfate aerosols
cloud radiative forcing
climate change
arctic summer cooling and winter warming
description The mechanisms behind Arctic warming and associated climate changes are difficult to discern. Also, the complex local processes and feedbacks like aerosol-cloud-climate interactions are yet to be quantified. Here, using the Community Earth System Model (CAM5) experiments, with emission enhancement of anthropogenic sulfate 1) five-fold globally, 2) ten-times over Asia, and 3) ten-times over Europe we show that regional emissions of sulfate aerosols alter seasonal warming over the Arctic, i.e., colder summer and warmer winter. European emissions play a dominant role in cooling during the summer season (0.7 K), while Asian emissions dominate the warming during the winter season (maximum ∼0.6 K) in the Arctic surface. The cooling/warming is associated with a negative/positive cloud radiative forcing. During the summer season increase in low–mid level clouds, induced by sulfate emissions, favours the solar dimming effect that reduces the downwelling radiation to the surface and thus leads to surface cooling. Warmer winters are associated with enhanced high-level clouds that induce a positive radiative forcing at the top of the atmosphere. This study points to the importance of international strategies being implemented to control sulfate emissions to combat air pollution. Such strategies will also affect the Arctic cooling/warming associated with a cloud radiative forcing caused by sulfate emission change.
format Conference Object
author Acharya Asutosh
Suvarna Fadnavis
M. Nuncio
Rolf Müller
Sarat C. Tripathy
author_facet Acharya Asutosh
Suvarna Fadnavis
M. Nuncio
Rolf Müller
Sarat C. Tripathy
author_sort Acharya Asutosh
title Presentation1_The Arctic Temperature Response to Global and Regional Anthropogenic Sulfate Aerosols.pdf
title_short Presentation1_The Arctic Temperature Response to Global and Regional Anthropogenic Sulfate Aerosols.pdf
title_full Presentation1_The Arctic Temperature Response to Global and Regional Anthropogenic Sulfate Aerosols.pdf
title_fullStr Presentation1_The Arctic Temperature Response to Global and Regional Anthropogenic Sulfate Aerosols.pdf
title_full_unstemmed Presentation1_The Arctic Temperature Response to Global and Regional Anthropogenic Sulfate Aerosols.pdf
title_sort presentation1_the arctic temperature response to global and regional anthropogenic sulfate aerosols.pdf
publishDate 2021
url https://doi.org/10.3389/fenvs.2021.766538.s001
https://figshare.com/articles/presentation/Presentation1_The_Arctic_Temperature_Response_to_Global_and_Regional_Anthropogenic_Sulfate_Aerosols_pdf/16947196
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
genre_facet Arctic
Climate change
op_relation doi:10.3389/fenvs.2021.766538.s001
https://figshare.com/articles/presentation/Presentation1_The_Arctic_Temperature_Response_to_Global_and_Regional_Anthropogenic_Sulfate_Aerosols_pdf/16947196
op_rights CC BY 4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.3389/fenvs.2021.766538.s001
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