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Gaubert B, Emmons LK, Raeder K, Tilmes S, Miyazaki K, Arellano AF, Elguindi N, Granier C, Tang W, Barré J, Worden HM, Buchholz RR, Edwards DP, Franke P, Anderson JL, Saunois M, Schroeder J, Woo JH, Simpson IJ, Blake DR, Meinardi S, Wennberg PO, Crounse J, Teng A, Kim M, Dickerson RR, He H, Ren X, Pusede SE, Diskin GS. Correcting model biases of CO in East Asia: impact on oxidant distributions during KORUS-AQ. ATMOSPHERIC CHEMISTRY AND PHYSICS 2020; 20:14617-14647. [PMID: 33414818 PMCID: PMC7786812 DOI: 10.5194/acp-20-14617-2020] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/05/2023]
Abstract
Global coupled chemistry-climate models underestimate carbon monoxide (CO) in the Northern Hemisphere, exhibiting a pervasive negative bias against measurements peaking in late winter and early spring. While this bias has been commonly attributed to underestimation of direct anthropogenic and biomass burning emissions, chemical production and loss via OH reaction from emissions of anthropogenic and biogenic volatile organic compounds (VOCs) play an important role. Here we investigate the reasons for this underestimation using aircraft measurements taken in May and June 2016 from the Korea-United States Air Quality (KORUS-AQ) experiment in South Korea and the Air Chemistry Research in Asia (ARIAs) in the North China Plain (NCP). For reference, multispectral CO retrievals (V8J) from the Measurements of Pollution in the Troposphere (MOPITT) are jointly assimilated with meteorological observations using an ensemble adjustment Kalman filter (EAKF) within the global Community Atmosphere Model with Chemistry (CAM-Chem) and the Data Assimilation Research Testbed (DART). With regard to KORUS-AQ data, CO is underestimated by 42% in the control run and by 12% with the MOPITT assimilation run. The inversion suggests an underestimation of anthropogenic CO sources in many regions, by up to 80% for northern China, with large increments over the Liaoning Province and the North China Plain (NCP). Yet, an often-overlooked aspect of these inversions is that correcting the underestimation in anthropogenic CO emissions also improves the comparison with observational O3 datasets and observationally constrained box model simulations of OH and HO2. Running a CAM-Chem simulation with the updated emissions of anthropogenic CO reduces the bias by 29% for CO, 18% for ozone, 11% for HO2, and 27% for OH. Longer-lived anthropogenic VOCs whose model errors are correlated with CO are also improved, while short-lived VOCs, including formaldehyde, are difficult to constrain solely by assimilating satellite retrievals of CO. During an anticyclonic episode, better simulation of O3, with an average underestimation of 5.5 ppbv, and a reduction in the bias of surface formaldehyde and oxygenated VOCs can be achieved by separately increasing by a factor of 2 the modeled biogenic emissions for the plant functional types found in Korea. Results also suggest that controlling VOC and CO emissions, in addition to widespread NO x controls, can improve ozone pollution over East Asia.
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Affiliation(s)
- Benjamin Gaubert
- Atmospheric Chemistry Observations and Modeling, National Center for Atmospheric Research, Boulder, CO, USA
| | - Louisa K. Emmons
- Atmospheric Chemistry Observations and Modeling, National Center for Atmospheric Research, Boulder, CO, USA
| | - Kevin Raeder
- Computational and Information Systems Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
| | - Simone Tilmes
- Atmospheric Chemistry Observations and Modeling, National Center for Atmospheric Research, Boulder, CO, USA
| | - Kazuyuki Miyazaki
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA
| | - Avelino F. Arellano
- Dept. of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ, USA
| | - Nellie Elguindi
- Laboratoire d’Aérologie, CNRS, Université de Toulouse, Toulouse, France
| | - Claire Granier
- Laboratoire d’Aérologie, CNRS, Université de Toulouse, Toulouse, France
- NOAA Chemical Sciences Laboratory-CIRES/University of Colorado, Boulder, CO, USA
| | - Wenfu Tang
- Advanced Study Program, National Center for Atmospheric Research, Boulder, CO, USA
| | - Jérôme Barré
- European Centre for Medium-Range Weather Forecasts, Shinfield Park, Reading, RG2 9AX, UK
| | - Helen M. Worden
- Atmospheric Chemistry Observations and Modeling, National Center for Atmospheric Research, Boulder, CO, USA
| | - Rebecca R. Buchholz
- Atmospheric Chemistry Observations and Modeling, National Center for Atmospheric Research, Boulder, CO, USA
| | - David P. Edwards
- Atmospheric Chemistry Observations and Modeling, National Center for Atmospheric Research, Boulder, CO, USA
| | - Philipp Franke
- Forschungszentrum Jülich GmbH, Institut für Energie und Klimaforschung IEK-8, 52425 Jülich, Germany
| | - Jeffrey L. Anderson
- Computational and Information Systems Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
| | - Marielle Saunois
- Laboratoire des Sciences du Climat et de l’Environnement, LSCE-IPSL (CEA-CNRS-UVSQ), Université Paris-Saclay, 91191 Gif-sur-Yvette, France
| | | | - Jung-Hun Woo
- Department of Advanced Technology Fusion, Konkuk University, Seoul, South Korea
| | - Isobel J. Simpson
- Department of Chemistry, University of California, Irvine, Irvine, CA 92697, USA
| | - Donald R. Blake
- Department of Chemistry, University of California, Irvine, Irvine, CA 92697, USA
| | - Simone Meinardi
- Department of Chemistry, University of California, Irvine, Irvine, CA 92697, USA
| | | | - John Crounse
- California Institute of Technology, Pasadena, CA, USA
| | - Alex Teng
- California Institute of Technology, Pasadena, CA, USA
| | - Michelle Kim
- California Institute of Technology, Pasadena, CA, USA
| | - Russell R. Dickerson
- Department of Atmospheric and Oceanic Science, University of Maryland, College Park, MD, USA
- Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USA
| | - Hao He
- Department of Atmospheric and Oceanic Science, University of Maryland, College Park, MD, USA
- Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USA
| | - Xinrong Ren
- Department of Atmospheric and Oceanic Science, University of Maryland, College Park, MD, USA
- Air Resources Laboratory, National Oceanic and Atmospheric Administration, College Park, MD, USA
| | - Sally E. Pusede
- Department of Environmental Sciences, University of Virginia, Charlottesville, VA, USA
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Hakami A, Henze DK, Seinfeld JH, Singh K, Sandu A, Kim S, Byun D, Li Q. The adjoint of CMAQ. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2007; 41:7807-17. [PMID: 18075092 DOI: 10.1021/es070944p] [Citation(s) in RCA: 12] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/11/2023]
Abstract
An adjoint model for the internationally used Community Multiscale Air Quality (CMAQ) modeling platform of the U.S. EPA is developed. The adjoint version for CMAQ (CMAQ-ADJ) provides the user community with forward (decoupled direct method or DDM) and backward (adjoint) sensitivity analysis capabilities. Current implementation is for gas-phase processes. Discrete adjoints are implemented for all processes with the exception of horizontal advection, for which, because of inherent discontinuities in the advection scheme, the continuous approach is superior. The adjoint of chemistry is constructed by interfacing CMAQ with the kinetic pre-processor, which provides for increased flexibility in the choice of chemical solver and facilitates the implementation of new chemical mechanisms. The adjoint implementation is evaluated both on a process-by-process basis and for the full model. In general, adjoint results show good agreement with brute-force and DDM sensitivities. As expected for a continuous adjoint implementation in a nonlinear scheme, the agreement is not perfect for horizontal transport. Sensitivities of various air quality, public health, and environmental metrics with respect to emissions are calculated using the adjoint method. In order to show applicability to regional climate studies, as an example, the sensitivities of these metrics with respect to local temperatures are calculated.
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Affiliation(s)
- Amir Hakami
- Department of Chemical Engineering, California Institute of Technology, 1200 E. California Boulevard, Pasadena, California 91125, USA
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