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The Role of Natural Halogens in Global Tropospheric Ozone Chemistry and Budget Under Different 21st Century Climate Scenarios

Authors :
Alba Badia
David W. Tarasick
Carlos A. Cuevas
Jane Liu
Fernando Iglesias-Suarez
Jean-Francois Lamarque
Paul T. Griffiths
Rafael P. Fernandez
Douglas E. Kinnison
Alfonso Saiz-Lopez
Apollo-University Of Cambridge Repository
European Commission
National Science Foundation (US)
Department of Energy (US)
Agencia Nacional de Promoción Científica y Tecnológica (Argentina)
Consejo Superior de Investigaciones Científicas (España)
Consejo Nacional de Investigaciones Científicas y Técnicas (Argentina)
Badia, A [0000-0003-0906-8258]
Iglesias-Suarez, F [0000-0003-3403-8245]
Fernandez, RP [0000-0002-4114-5500]
Cuevas, CA [0000-0002-9251-5460]
Kinnison, DE [0000-0002-3418-0834]
Lamarque, JF [0000-0002-4225-5074]
Griffiths, PT [0000-0002-1089-340X]
Tarasick, DW [0000-0001-9869-0692]
Liu, J [0000-0001-7760-2788]
Saiz-Lopez, A [0000-0002-0060-1581]
Apollo - University of Cambridge Repository
Source :
Digital.CSIC. Repositorio Institucional del CSIC, instname
Publication Year :
2021
Publisher :
Apollo - University of Cambridge Repository, 2021.

Abstract

25 pags., 14 figs., 2 tabs.<br />Tropospheric ozone ((Formula presented.)) is an important greenhouse gas and a surface pollutant. The future evolution of (Formula presented.) abundances and chemical processing are uncertain due to a changing climate, socioeconomic developments, and missing chemistry in global models. Here, we use an Earth System Model with natural halogen chemistry to investigate the changes in the (Formula presented.) budget over the 21st century following Representative Concentration Pathway (RCP)6.0 and RCP8.5 climate scenarios. Our results indicate that the global tropospheric (Formula presented.) net chemical change (NCC, chemical gross production minus destruction) will decrease (Formula presented.), notwithstanding increasing or decreasing trends in ozone production and loss. However, a wide range of surface NCC variations (from −60 (Formula presented.) to 150 (Formula presented.)) are projected over polluted regions with stringent abatements in (Formula presented.) precursor emissions. Water vapor and iodine are found to be key drivers of future tropospheric (Formula presented.) destruction, while the largest changes in (Formula presented.) production are determined by the future evolution of peroxy radicals. We show that natural halogens, currently not considered in climate models, significantly impact on the present-day and future global (Formula presented.) burden reducing (Formula presented.) 30–35 Tg (11–15 (Formula presented.)) of tropospheric ozone throughout the 21st century regardless of the RCP scenario considered. This highlights the importance of including natural halogen chemistry in climate model projections of future tropospheric ozone.<br />EC, H2020, H2020 Priority Excellent Science, H2020 European Research Council (ERC). Grant Number: ERC-2016-COG726349; NSF, Office of Science of the US Department of Energy, PICT-2016-0714 (ANPCyT) i-COOP-B20331 (CSIC + CONICET)

Subjects

Subjects :
010504 meteorology & atmospheric sciences
Radio oceanography
01 natural sciences
7. Clean energy
ATMOSPHERIC PROCESSES
Climate change and variability
Oceans
Earth and Planetary Sciences (miscellaneous)
Cryosphere
Sea level change
Water cycle
OCEANOGRAPHY: PHYSICAL
General circulation
Regional modeling
Atmospheric effects
Hydrological cycles and budgets
Gravity and isostasy
climate change
Geophysics
RADIO SCIENCE
Global climate models
Land/atmosphere interactions
Global change from geodesy
Atmospheric
Climate impact
Mud volcanism
Volcano monitoring
MARINE GEOLOGY AND GEOPHYSICS
CRYOSPHERE
chemistry
Earthquake ground motions and engineering seismology
Effusive volcanism
HYDROLOGY
Earth System Model
Sea level: variations and mean
Tropospheric ozone
Climate variability
climate
Solid Earth
Pollutant
Tsunamis and storm surges
VOLCANOLOGY
COMPUTATIONAL GEOPHYSICS
Geological
Ocean/Earth/atmosphere/hydrosphere/cryosphere interactions
Atmosphere
Volcano seismology
SEISMOLOGY
Modeling
Benefit‐cost analysis
Global change
Composition and Chemistry
Avalanches
NATURAL HAZARDS
Abrupt/rapid climate change
ozone
Biosphere/atmosphere interactions
Space and Planetary Science
Greenhouse gas
Volcanic effects
Atmospheric Science
Ocean monitoring with geodetic techniques
010501 environmental sciences
Mass balance
Atmospheric sciences
Climate dynamics
Air/sea interactions
Regional climate change
chemistry.chemical_compound
INFORMATICS
Numerical modeling
emission
Surface waves and tides
Earth system modeling
PALEOCEANOGRAPHY
Explosive volcanism
GEODESY AND GRAVITY
Climatology
Physical modeling
Decadal ocean variability
POLICY SCIENCES
Ocean/atmosphere interactions
Volcano/climate interactions
Climate and interannual variability
Impacts of global change
OCEANOGRAPHY: GENERAL
Disaster risk analysis and assessment
Research Article
Climate impacts
Risk
Ozone
Troposphere: composition and chemistry
Air/sea constituent fluxes
Oceanic
TECTONOPHYSICS
Numerical solutions
modelling
Volcanic hazards and risks
Evolution of the Earth
halogens
halogen chemistry
GLOBAL CHANGE
ATMOSPHERIC COMPOSITION AND STRUCTURE
0105 earth and related environmental sciences
BIOGEOSCIENCES
Water cycles
Ocean influence of Earth rotation
13. Climate action
Evolution of the atmosphere
Climate model
Theoretical modeling

Details

Database :
OpenAIRE
Journal :
Digital.CSIC. Repositorio Institucional del CSIC, instname
Accession number :
edsair.doi.dedup.....37e32f0d7e0e9f7dd81d776654307904
Full Text :
https://doi.org/10.17863/cam.77077