Quantifying the causes of differences in tropospheric OH within global models. Issue 3 (10th February 2017)

• Record Type: Journal Article
• Authors: Nicely, Julie M.; Salawitch, Ross J.; Canty, Timothy; Anderson, Daniel C.; Arnold, Steve R.; Chipperfield, Martyn P.; Emmons, Louisa K.; Flemming, Johannes; Huijnen, Vincent; Kinnison, Douglas E.; Lamarque, Jean‐François; Mao, Jingqiu; Monks, Sarah A.; Steenrod, Stephen D.; Tilmes, Simone; Turquety, Solene
• Is Part Of: Journal of geophysical research. Volume 122:Issue 3(2017)
• Page Start: 1983
• Page End: 2007
• Publication Date: 2017-02-10
• Subjects: hydroxyl radical -- tropospheric chemistry -- methane lifetime -- POLMIP -- OH -- oxidizing capacity; Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1002/2016JD026239
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: The hydroxyl radical (OH) is the primary daytime oxidant in the troposphere and provides the main loss mechanism for many pollutants and greenhouse gases, including methane (CH4 ). Global mean tropospheric OH differs by as much as 80% among various global models, for reasons that are not well understood. We use neural networks (NNs), trained using archived output from eight chemical transport models (CTMs) that participated in the Polar Study using Aircraft, Remote Sensing, Surface Measurements and Models, of Climate, Chemistry, Aerosols and Transport Model Intercomparison Project (POLMIP), to quantify the factors responsible for differences in tropospheric OH and resulting CH4 lifetime ( τ CH4 ) between these models. Annual average τ CH4, for loss by OH only, ranges from 8.0 to 11.6 years for the eight POLMIP CTMs. The factors driving these differences were quantified by inputting 3‐D chemical fields from one CTM into the trained NN of another CTM. Across all CTMs, the largest mean differences in τ CH4 (Δ τ CH4 ) result from variations in chemical mechanisms (Δ τ CH4 = 0.46 years), the photolysis frequency ( J ) of O3 → O( 1 D) (0.31 years), local O3 (0.30 years), and CO (0.23 years). The Δ τ CH4 due to CTM differences in NO x (NO + NO2 ) is relatively low (0.17 years), although large regional variation in OH between the CTMs is attributed to NO x . Differences in isoprene and J (NO2 ) have negligible overall effect on globally averaged tropospheric OH, although the extent of OH variations due to each factor depends on the model being examined. This study demonstrates that NNs can serve as a useful tool for quantifying why tropospheric OH varies between global models, provided that essential chemical fields are archived. Key Points: Factors responsible for OH and CH4 lifetime differences between eight models are quantified by using neural networks O3, the photolysis frequency ( J ) of O3 to O( 1 D), CO, and chemical mechanism differences are main drivers of OH variations H2 O and NO x differences drive moderate OH variation on regional scale; isoprene and J (NO2 ) differences have small role in driving OH variations