Tomás Sherwen, Mat Evans, Lucy Carpenter Wolfson Atmospheric Chemistry Laboratories, University of York, UK CAST Science team. Rainer Volkamer (c), Theodore.

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Presentation transcript:

Tomás Sherwen, Mat Evans, Lucy Carpenter Wolfson Atmospheric Chemistry Laboratories, University of York, UK CAST Science team. Rainer Volkamer (c), Theodore Koenig (c), Barbara Dix (c), Carlos Ordonez (d), Alfonso Saiz-Lopez (d) b National Centre for Atmospheric Science (NCAS), Department of Chemistry, University of York, UK c Cooperative Institute for Research in Environmental Sciences (CIRES), Department of Chemistry and Biochemistry, University of Colorado, CO, USA d Atmospheric Chemistry and Climate Group (AC2), Instituto de Química Física Rocasolano, CSIC, Madrid, Spain Modelling global atmospheric iodine.

Image: Saiz-Lopez et al., 2012 Tropospheric Iodine HOI

GEOS-Chem GEOS-Chem v9-2 Standard 66 tracers Chemistry ~270 reactions 47 Levels up to ~80 km Bromine chemistry scheme (Parrella, 2012) NB Not with Johan’s updates New work included emissions, chemistry, deposition of I

Organic emissions Ordonez et al., 2012

Inorganic emissions HOI (nmol m -2 day -1 ) I 2 (nmol m -2 day -1 ) Ocean emission of HOI and I 2 (Carpenter et al., 2013) Parameterized using O 3, 10m wind, oceanic iodide from SST (Chance et al., 2014)

Chemistry HOI

Precursor gases: CH 2 ICl CH 2 ICl

Precursor gases: CH 3 I CH 3 I

Column IO

Observations Reactive Iodine

Surface IO Model Measurements Model Latitude IO (pptv) 0 2 1

Vertical IO TORERO

Vertical iodine composition IONO2 IO I2I2 HOI CH 3 I

O 3 Change with just iodine 14 Screenshot

15 O 3 Change with just bromine

16 O 3 Change with halogens

Global ozone loss HO 2 +O 3 OH+O 3 O 3 +hv+H 2 O Iodine Bromine

Impact of halogens on global oxidation Two influencers O 3  OH  XO+HO 2  HOX+h  OH+X OH  OH Mass weighted global Just Br -2.7% Just I +0.1% Both -2.5% CH 4 lifetime Just Br +2.8% Just I -0.04% Both +2.6%

Chemical uncertainties: IO

CONTRAST / CAST

Conclusions Building a reactive iodine simulations Very poorly constrained by observations Often poorly defined kinetics Rather suprisinly IO concentrations calculated are consistent with observations Iodine alone ~2-7% change in O 3 column Iodine has almost no impact on OH Halogens ~10% change in O 3 column