TY - JOUR
T1 - Intercomparison Between Surrogate, Explicit, and Full Treatments of VSL Bromine Chemistry Within the CAM-Chem Chemistry-Climate Model
AU - Fernandez, Rafael P.
AU - Barrera, Javier A.
AU - López-Noreña, Ana Isabel
AU - Kinnison, Douglas E.
AU - Nicely, Julie
AU - Salawitch, Ross J.
AU - Wales, Pamela A.
AU - Toselli, Beatriz M.
AU - Tilmes, Simone
AU - Lamarque, Jean François
AU - Cuevas, Carlos A.
AU - Saiz-Lopez, Alfonso
N1 - Publisher Copyright:
© 2020. The Authors.
PY - 2021/2/28
Y1 - 2021/2/28
N2 - Many 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.
AB - Many 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.
KW - CAM-Chem
KW - CCMI
KW - lowermost stratospheric ozone
KW - tropospheric oxidation capacity
KW - very-short lived bromine
UR - https://www.scopus.com/pages/publications/85101744522
U2 - 10.1029/2020GL091125
DO - 10.1029/2020GL091125
M3 - Article
AN - SCOPUS:85101744522
SN - 0094-8276
VL - 48
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 4
M1 - e2020GL091125
ER -