Better representation of dust can improve climate models with too weak an African monsoon
<p>The amount of short wave radiation absorbed by dust has remained uncertain. We have developed a more accurate representation of dust absorption that is based on the observed dust mineralogical composition and accounts for very large particles. We analyze the results from two fully coupled c...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2021-07-01
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| Series: | Atmospheric Chemistry and Physics |
| Online Access: | https://acp.copernicus.org/articles/21/11423/2021/acp-21-11423-2021.pdf |
| _version_ | 1819090121736060928 |
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| author | Y. Balkanski R. Bonnet O. Boucher R. Checa-Garcia J. Servonnat |
| author_facet | Y. Balkanski R. Bonnet O. Boucher R. Checa-Garcia J. Servonnat |
| author_sort | Y. Balkanski |
| collection | DOAJ |
| description | <p>The amount of short wave radiation absorbed by dust has remained
uncertain. We have developed a more accurate representation of dust
absorption that is based on the observed dust mineralogical composition and
accounts for very large particles. We analyze the results from two
fully coupled climate simulations of 100 years in terms of their simulated
precipitation patterns against observations. A striking benefit of the new
dust optical and physical properties is that tropical precipitation over the Sahel, tropical North Atlantic and West Indian Ocean are significantly
improved compared to observations, without degrading precipitations
elsewhere. This alleviates a common persistent bias in Earth system models
that exhibit a summer African monsoon that does not reach far enough north.
We show that the improvements documented here for the IPSL-CM6<span class="note-anchor" id="fna_Ch1.Footn1"><a href="#fn_Ch1.Footn1"><sup>1</sup></a></span> climate model result from both a thermodynamical and dynamical response to dust
absorption, which is unrelated to natural variability. Aerosol absorption
induces more water vapor advection from the ocean to the Sahel region,
thereby providing an added supply of moisture available for precipitation.
This work, thus, provides a path towards improving precipitation patterns in these regions by accounting for both physical and optical properties of the aerosol more realistically.</p> |
| first_indexed | 2024-12-21T22:18:48Z |
| format | Article |
| id | doaj.art-a89f8f4a0b064923b52052c8f3cb6bd9 |
| institution | Directory Open Access Journal |
| issn | 1680-7316 1680-7324 |
| language | English |
| last_indexed | 2024-12-21T22:18:48Z |
| publishDate | 2021-07-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Atmospheric Chemistry and Physics |
| spelling | doaj.art-a89f8f4a0b064923b52052c8f3cb6bd92022-12-21T18:48:24ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242021-07-0121114231143510.5194/acp-21-11423-2021Better representation of dust can improve climate models with too weak an African monsoonY. Balkanski0R. Bonnet1O. Boucher2R. Checa-Garcia3J. Servonnat4Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ, IPSL, Gif-sur-Yvette, FranceInstitut Pierre-Simon Laplace, Sorbonne Université-CNRS, Paris, FranceInstitut Pierre-Simon Laplace, Sorbonne Université-CNRS, Paris, FranceLaboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ, IPSL, Gif-sur-Yvette, FranceLaboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ, IPSL, Gif-sur-Yvette, France<p>The amount of short wave radiation absorbed by dust has remained uncertain. We have developed a more accurate representation of dust absorption that is based on the observed dust mineralogical composition and accounts for very large particles. We analyze the results from two fully coupled climate simulations of 100 years in terms of their simulated precipitation patterns against observations. A striking benefit of the new dust optical and physical properties is that tropical precipitation over the Sahel, tropical North Atlantic and West Indian Ocean are significantly improved compared to observations, without degrading precipitations elsewhere. This alleviates a common persistent bias in Earth system models that exhibit a summer African monsoon that does not reach far enough north. We show that the improvements documented here for the IPSL-CM6<span class="note-anchor" id="fna_Ch1.Footn1"><a href="#fn_Ch1.Footn1"><sup>1</sup></a></span> climate model result from both a thermodynamical and dynamical response to dust absorption, which is unrelated to natural variability. Aerosol absorption induces more water vapor advection from the ocean to the Sahel region, thereby providing an added supply of moisture available for precipitation. This work, thus, provides a path towards improving precipitation patterns in these regions by accounting for both physical and optical properties of the aerosol more realistically.</p>https://acp.copernicus.org/articles/21/11423/2021/acp-21-11423-2021.pdf |
| spellingShingle | Y. Balkanski R. Bonnet O. Boucher R. Checa-Garcia J. Servonnat Better representation of dust can improve climate models with too weak an African monsoon Atmospheric Chemistry and Physics |
| title | Better representation of dust can improve climate models with too weak an African monsoon |
| title_full | Better representation of dust can improve climate models with too weak an African monsoon |
| title_fullStr | Better representation of dust can improve climate models with too weak an African monsoon |
| title_full_unstemmed | Better representation of dust can improve climate models with too weak an African monsoon |
| title_short | Better representation of dust can improve climate models with too weak an African monsoon |
| title_sort | better representation of dust can improve climate models with too weak an african monsoon |
| url | https://acp.copernicus.org/articles/21/11423/2021/acp-21-11423-2021.pdf |
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