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M. Kanakidou, F. Dentener, G. Brasseur, T. Berntsen, W. Collins, D. Hauglustaine, S. Houweling, I. Isaksen, M. Krol, M. Lawrence, J. Müller, N. Poisson, G. Roelofs, Yuxuan Wang, W. Wauben (1999)
3-D global simulations of tropospheric CO distributions - results of the GIM/IGAC intercomparison 1997 exerciseChemosphere - Global Change Science, 1
DS Stevenson, WJ Collins, CE Johnson, R. Derwent (1998)
Intercomparison and evaluation of atmospheric transport in a Lagrangian model (STOCHEM), and an Eulerian model (UM), using 222Rn as a short‐lived tracerQuarterly Journal of the Royal Meteorological Society, 124
H. Nuesser, H. Reichow, C. Winter, H. Grieb, P. Crutzen, D. Wuebbles, H. Grassl, P. Fabian, U. Schumann, K. Liou (1990)
Proceedings of the DLR International Colloquium on Air Traffic and the Environment - Background, Tendencies and Potential Global Atmospheric Effects
G. Watts (1998)
Climate Change 1995Pacific Conservation Biology, 4
J. Olson, M. Prather, T. Berntsen, G. Carmichael, R. Chatfield, P. Connell, R. Derwent, L. Horowitz, Shengxin Jin, M. Kanakidou, P. Kasibhatla, R. Kotamarthi, M. Kuhn, K. Law, J. Penner, Lori Perliski, S. Sillman, F. Stordal, A. Thompson, O. Wild (1997)
Results from the Intergovernmental Panel on Climatic Change Photochemical Model Intercomparison (PhotoComp)Journal of Geophysical Research, 102
R. Dorland, F. Dentener, J. Lelieveld (1997)
Radiative forcing due to tropospheric ozone and sulfate aerosolsJournal of Geophysical Research, 102
P. Forster, Colin Johnson, K. Law, J. Pyle, K. Shine (1996)
Further estimates of radiative forcing due to tropospheric ozone changesGeophysical Research Letters, 23
W. Collins, D. Stevenson, C. Johnson, R. Derwent (1997)
Tropospheric Ozone in a Global-Scale Three-Dimensional Lagrangian Model and Its Response to NOX Emission ControlsJournal of Atmospheric Chemistry, 26
J. Edwards, A. Slingo (1996)
Studies with a flexible new radiation code. I: Choosing a configuration for a large-scale modelQuarterly Journal of the Royal Meteorological Society, 122
Kanakidou Kanakidou (1998)
3‐D global simulations of tropospheric O3 budget ‐ results of the GIM/IGAC intercomparison 1997 exerciseAnnales Geophysicae, 16
(1980)
Nitrogen and Sulfur Oxides
J. Dignon, S. Hameed (1989)
GLOBAL EMISSIONS OF NITROGEN AND SULFUR OXIDES FROM 1860 TO 1980Journal of the Air Pollution Control Association, 39
J. Lelieveld, R. Dorland (1995)
Ozone chemistry changes in the troposphere and consequent radiative forcing of climate.
Johnson Johnson, Derwent Derwent (1996)
Relative radiative forcing consequences of global emissions of hydrocarbons, CO and NOx from human activities estimated with a zonally‐averaged 2‐D modelClimatic Change, 34
G. Roelofs, J. Lelieveld, R. Dorland (1997)
A three-dimensional chemistry/general circulation model simulation of anthropogenically derived ozone in the troposphere and its radiative climate forcingJournal of Geophysical Research, 102
J. Houghton, B. Callander, S. Varney (1992)
Climate change 1992 : the supplementary report to the IPCC scientific assessment
J. Houghton (1992)
Climate Change 1992
(1995)
A 4-D ozone climatology for UGAMP models
Derwent, Intercomparison and evaluation of atmospheric transport
G. Brasseur, J. Kiehl, J. Müller, T. Schneider, C. Granier, X. Tie, D. Hauglustaine (1998)
Past and future changes in global tropospheric ozone: Impact on radiative forcingGeophysical Research Letters, 25
A. Marenco, H. Gouget, P. Nédélec, J. Pages, F. Karcher (1994)
Evidence of a long‐term increase in tropospheric ozone from Pic du Midi data series: Consequences: Positive radiative forcingJournal of Geophysical Research, 99
C. Senior (1999)
Comparison of Mechanisms of Cloud-Climate Feedbacks in GCMsJournal of Climate, 12
K. Shine, B. Briegleb, A. Grossman, D. Hauglustaine, H. Mao, V. Ramaswamy, M. Schwarzkopf, R. Dorland, Wei‐Chyung Wang (1995)
Radiative forcing due to changes in ozone: a comparison of different codes
(1995)
The Science of Climate Change, edited by J
H. Reichow (1990)
Fuel Consumption and Emissions of Air Traffic
C. Johnson, R. Derwent (1996)
Relative radiative forcing consequences of global emissions of hydrocarbons, carbon monoxide and NOx from human activities estimated with a zonally-averaged two-dimensional modelClimatic Change, 34
D. Hauglustaine, C. Granier, G. Brasseur, G. Mégie (1994)
The importance of atmospheric chemistry in the calculation of radiative forcing on the climate systemJournal of Geophysical Research, 99
T. Berntsen, I. Isaksen, G. Myhre, J. Fuglestvedt, F. Stordal, T. Larsen, R. Freckleton, K. Shine (1997)
Effects of anthropogenic emissions on tropospheric ozone and its radiative forcingJournal of Geophysical Research, 102
E. Harrison, P. Minnis, B. Barkstrom, V. Ramanathan, R. Cess, G. Gibson (1990)
Seasonal variation of cloud radiative forcing derived from the Earth Radiation Budget ExperimentJournal of Geophysical Research, 95
S. Oltmans, A. Lefohn, H. Scheel, J. Harris, H. Levy, I. Galbally, E. Brunke, C. Meyer, J. Lathrop, Beverly Johnson, D. Shadwick, E. Cuevas, F. Schmidlin, D. Tarasick, H. Claude, J. Kerr, O. Uchino, V. Mohnen (1998)
Trends of ozone in the troposphereGeophysical Research Letters, 25
T. Johns, R. Carnell, J. Crossley, J. Gregory, J. Mitchell, C. Senior, S. Tett, R. Wood (1997)
The second Hadley Centre coupled ocean-atmosphere GCM: model description, spinup and validationClimate Dynamics, 13
We present the first estimate of the evolution of tropospheric ozone (O3(T)) radiative forcing since 1860 and into the future. The UKMO 3‐D chemistry‐transport model (STOCHEM) was used to simulate the tropospheric composition in 1860, 1950, 1970, 1990 and 2100, by changing trace gas emissions. The future scenario used a doubled CO2 climate. STOCHEM includes extensive non‐methane hydrocarbon (NMHC) chemistry, and produces a reasonable simulation of present‐day O3(T). Radiative forcings caused by the modelled changes in O3(T) since 1860 were calculated using the UKMO radiation code, and included clouds and stratospheric temperature adjustment. Calculated changes in the global annual mean forcing since 1860 were 0.13, 0.22, 0.29 and 0.48 W m−2 for the four years. Up to 1990 this forcing scales linearly with the change in total NOx emissions since 1860; this linearity breaks down in 2100. The 1990 forcing is at the lower end of the range from previous modelling studies (0.28–0.51 W m−2), but is still significant, enhancing the well‐mixed greenhouse gas forcing by over 10%.
Geophysical Research Letters – Wiley
Published: Oct 15, 1998
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