Critical role of biomass burning aerosols in enhanced historical Indian Ocean warming

Abstract The tropical Indian Ocean (TIO) has experienced enhanced surface warming relative to the tropical mean during the past century, but the underlying mechanisms remain unclear. Here we use single-forcing, large-ensemble coupled model simulations to demonstrate that changes of biomass burning (...

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Main Authors: Yiqun Tian, Shineng Hu, Clara Deser
Format: Article
Language:English
Published: Nature Portfolio 2023-06-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-023-39204-y
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author Yiqun Tian
Shineng Hu
Clara Deser
author_facet Yiqun Tian
Shineng Hu
Clara Deser
author_sort Yiqun Tian
collection DOAJ
description Abstract The tropical Indian Ocean (TIO) has experienced enhanced surface warming relative to the tropical mean during the past century, but the underlying mechanisms remain unclear. Here we use single-forcing, large-ensemble coupled model simulations to demonstrate that changes of biomass burning (BMB) aerosols have played a critical role in this TIO relative warming. Although the BMB aerosol changes have little effect on global mean temperatures due to regional cancellation, they significantly influence the pattern of warming over the tropical oceans. The reduction of BMB aerosols over the Indian subcontinent induces a TIO warming, while the increase of BMB aerosols over South America and Africa causes a cooling of the tropical Pacific and Atlantic, respectively. The resultant TIO relative warming leads to prominent global climate changes, including a westward expanded Indo-Pacific warm pool, a fresher TIO due to enhanced rainfall, and an intensified North Atlantic jet stream affecting European hydroclimate.
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spelling doaj.art-25399b8dee174077992e4ed82772e3a82023-06-18T11:18:53ZengNature PortfolioNature Communications2041-17232023-06-011411810.1038/s41467-023-39204-yCritical role of biomass burning aerosols in enhanced historical Indian Ocean warmingYiqun Tian0Shineng Hu1Clara Deser2Division of Earth and Climate Sciences, Nicholas School of the Environment, Duke UniversityDivision of Earth and Climate Sciences, Nicholas School of the Environment, Duke UniversityClimate and Global Dynamics, National Center for Atmospheric ResearchAbstract The tropical Indian Ocean (TIO) has experienced enhanced surface warming relative to the tropical mean during the past century, but the underlying mechanisms remain unclear. Here we use single-forcing, large-ensemble coupled model simulations to demonstrate that changes of biomass burning (BMB) aerosols have played a critical role in this TIO relative warming. Although the BMB aerosol changes have little effect on global mean temperatures due to regional cancellation, they significantly influence the pattern of warming over the tropical oceans. The reduction of BMB aerosols over the Indian subcontinent induces a TIO warming, while the increase of BMB aerosols over South America and Africa causes a cooling of the tropical Pacific and Atlantic, respectively. The resultant TIO relative warming leads to prominent global climate changes, including a westward expanded Indo-Pacific warm pool, a fresher TIO due to enhanced rainfall, and an intensified North Atlantic jet stream affecting European hydroclimate.https://doi.org/10.1038/s41467-023-39204-y
spellingShingle Yiqun Tian
Shineng Hu
Clara Deser
Critical role of biomass burning aerosols in enhanced historical Indian Ocean warming
Nature Communications
title Critical role of biomass burning aerosols in enhanced historical Indian Ocean warming
title_full Critical role of biomass burning aerosols in enhanced historical Indian Ocean warming
title_fullStr Critical role of biomass burning aerosols in enhanced historical Indian Ocean warming
title_full_unstemmed Critical role of biomass burning aerosols in enhanced historical Indian Ocean warming
title_short Critical role of biomass burning aerosols in enhanced historical Indian Ocean warming
title_sort critical role of biomass burning aerosols in enhanced historical indian ocean warming
url https://doi.org/10.1038/s41467-023-39204-y
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AT claradeser criticalroleofbiomassburningaerosolsinenhancedhistoricalindianoceanwarming