dc.creatorFernandez, Rafael Pedro
dc.creatorBarrera, Javier Alejandro
dc.creatorLopez Noreña, Ana Isabel
dc.creatorKinnison, Douglas E.
dc.creatorNicely, Julie M.
dc.creatorSalawitch, Ross J.
dc.creatorWales, Pamela A.
dc.creatorToselli, Beatriz Margarita
dc.creatorTilmes, Simone
dc.creatorLamarque, Jean François
dc.creatorCuevas, Carlos Alberto
dc.creatorSaiz López, Alfonso
dc.date.accessioned2022-09-07T18:22:21Z
dc.date.accessioned2022-10-15T08:33:01Z
dc.date.available2022-09-07T18:22:21Z
dc.date.available2022-10-15T08:33:01Z
dc.date.created2022-09-07T18:22:21Z
dc.date.issued2021-02
dc.identifierFernandez, Rafael Pedro; Barrera, Javier Alejandro; Lopez Noreña, Ana Isabel; Kinnison, Douglas E.; Nicely, Julie M.; et al.; Intercomparison between surrogate, explicit, and full treatments of VSL bromine chemistry within the CAM-Chem chemistry-climate model; American Geophysical Union; Geophysical Research Letters; 48; 4; 2-2021; 1-10
dc.identifier0094-8276
dc.identifierhttp://hdl.handle.net/11336/167805
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4365439
dc.description.abstractMany Chemistry-Climate Models (CCMs) include a simplified treatment of brominated very short-lived (VSLBr) species by assuming CH3Br as a surrogate for VSLBr. However, neglecting a comprehensive treatment of VSLBr in CCMs may yield an unrealistic representation of the associated impacts. Here, we use the Community Atmospheric Model with Chemistry (CAM-Chem) CCM to quantify the tropospheric and stratospheric changes between various VSLBr chemical approaches with increasing degrees of complexity (i.e., surrogate, explicit, and full). Our CAM-Chem results highlight the improved accuracy achieved by considering a detailed treatment of VSLBr photochemistry, including sea-salt aerosol dehalogenation and heterogeneous recycling on ice-crystals. Differences between the full and surrogate schemes maximize in the lowermost stratosphere and midlatitude free troposphere, resulting in a latitudinally dependent reduction of ∼1–7 DU in total ozone column and a ∼5%–15% decrease of the OH/HO2 ratio. We encourage all CCMs to include a complete chemical treatment of VSLBr in the troposphere and stratosphere.
dc.languageeng
dc.publisherAmerican Geophysical Union
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020GL091125
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1029/2020GL091125
dc.rightshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/
dc.rightsinfo:eu-repo/semantics/openAccess
dc.subjectCAM-CHEM
dc.subjectCCMI
dc.subjectLOWERMOST STRATOSPHERIC OZONE
dc.subjectTROPOSPHERIC OXIDATION CAPACITY
dc.subjectVERY-SHORT LIVED BROMINE
dc.titleIntercomparison between surrogate, explicit, and full treatments of VSL bromine chemistry within the CAM-Chem chemistry-climate model
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:ar-repo/semantics/artículo
dc.typeinfo:eu-repo/semantics/publishedVersion


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