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Papers by J. McConnell
Physical Review C, 1999
ABSTRACT
Physical Review C, 1973
... Phys. 7, 1 (1968)]. JF Mason and MW Johns, Can. J. Phys. 48, 2895 (1970) [INSPEC][ADS]. RJ Ol... more ... Phys. 7, 1 (1968)]. JF Mason and MW Johns, Can. J. Phys. 48, 2895 (1970) [INSPEC][ADS]. RJ Olson, WL Talbert, Jr., and JR McConnell, Phys. Rev. ... 26J. F. Mason and MW Johns, Can. J. Phys. 48, 2895 (1970). 27R. J. Olson, WL Talbert, Jr., and JR McConnell, Phys. Rev. ...
Journal of Geophysical Research, 1999
The Canadian Regional Climate Model with oxidant chemistry (CRCM) has been used to study the clim... more The Canadian Regional Climate Model with oxidant chemistry (CRCM) has been used to study the climatology and transport of ground-level ozone in eastern North America. The climatology is derived from simulations of five consecutive Julys from 1990 to 1994. Biogenic emissions are calculated each time step, while anthropogenic emissions are taken to be identical for each simulated July. Comparisons of daily ozone maximum for each individual month suggest that the model is simulating satisfactorily the month-long periods and usually correctly reproduces the high and low ozone regimes associated with the different parts of the domain and/or the various synoptic conditions, the Ohio region being the exception.
Journal of Geophysical Research, 1999
The Canadian Regional Climate Model with oxidant chemistry (CRCM) has been used to study the clim... more The Canadian Regional Climate Model with oxidant chemistry (CRCM) has been used to study the climatology and transport of ground-level ozone in eastern North America. The climatology is derived from simulations of five consecutive Julys from 1990 to 1994. Biogenic emissions are calculated each time step, while anthropogenic emissions are taken to be identical for each simulated July. Comparisons of daily ozone maximum for each individual month suggest that the model is simulating satisfactorily the month-long periods and usually correctly reproduces the high and low ozone regimes associated with the different parts of the domain and/or the various synoptic conditions, the Ohio region being the exception.
Physical Review C, 1999
ABSTRACT
Physical Review C, 1973
... Phys. 7, 1 (1968)]. JF Mason and MW Johns, Can. J. Phys. 48, 2895 (1970) [INSPEC][ADS]. RJ Ol... more ... Phys. 7, 1 (1968)]. JF Mason and MW Johns, Can. J. Phys. 48, 2895 (1970) [INSPEC][ADS]. RJ Olson, WL Talbert, Jr., and JR McConnell, Phys. Rev. ... 26J. F. Mason and MW Johns, Can. J. Phys. 48, 2895 (1970). 27R. J. Olson, WL Talbert, Jr., and JR McConnell, Phys. Rev. ...
Journal of Geophysical Research, 1999
The Canadian Regional Climate Model with oxidant chemistry (CRCM) has been used to study the clim... more The Canadian Regional Climate Model with oxidant chemistry (CRCM) has been used to study the climatology and transport of ground-level ozone in eastern North America. The climatology is derived from simulations of five consecutive Julys from 1990 to 1994. Biogenic emissions are calculated each time step, while anthropogenic emissions are taken to be identical for each simulated July. Comparisons of daily ozone maximum for each individual month suggest that the model is simulating satisfactorily the month-long periods and usually correctly reproduces the high and low ozone regimes associated with the different parts of the domain and/or the various synoptic conditions, the Ohio region being the exception.
Journal of Geophysical Research, 1999
The Canadian Regional Climate Model with oxidant chemistry (CRCM) has been used to study the clim... more The Canadian Regional Climate Model with oxidant chemistry (CRCM) has been used to study the climatology and transport of ground-level ozone in eastern North America. The climatology is derived from simulations of five consecutive Julys from 1990 to 1994. Biogenic emissions are calculated each time step, while anthropogenic emissions are taken to be identical for each simulated July. Comparisons of daily ozone maximum for each individual month suggest that the model is simulating satisfactorily the month-long periods and usually correctly reproduces the high and low ozone regimes associated with the different parts of the domain and/or the various synoptic conditions, the Ohio region being the exception.