| |
CO2
|
CH4
|
CFC-11
|
CFC-12
|
N2O
|
|
Preindustrial atmospheric concentration
|
280 ppmv
|
0.8 ppmv
|
0
|
0
|
288 ppbv
|
|
Current atmospheric concentration (1990)a
|
353 ppmv
|
1.72 ppmv
|
280 pptv
|
484 pptv
|
310 ppbv
|
|
Current rate of annual atmospheric
accumulationb
|
1.8 ppmv (0.5%)
|
0.015 ppmv (0.9%)
|
9.5 pptv (4%)
|
17 pptv (4%)
|
0.8 ppbv (0.25%)
|
|
Atmospheric lifetime (years>c
|
(50–200)
|
10
|
65
|
130
|
150
|
|
NOTE: Ozone has not been included in the table
because of lack of precise data. Here ppmv = parts per million by
volume, ppbv = parts per billion by volume, and pptv = parts per
trillion by volume.
|
|
aThe 1990
concentrations have been estimated on the basis of an extrapolation
of measurements reported for earlier years, assuming that the
recent trends remained approximately constant.
|
|
bNet
annual emissions of CO2 from the
biosphere not affected by human activity, such as volcanic
emissions, are assumed to be small. Estimates of human-induced
emissions from the biosphere are controversial.
|
|
cFor each
gas in the table, except CO2, the
''lifetime" is defined as the ratio of the atmospheric
concentration to the total rate of removal. This time scale also
characterizes the rate of adjustment of the atmospheric
concentrations if the emission rates are changed abruptly. CO2 is a special case because it is merely
circulated among various reservoirs (atmosphere, ocean, biota). The
"lifetime" of CO2 given in the table
is a rough indication of the time it would take for the CO2 concentration to adjust to changes in
the emissions.
|
|
SOURCE: Intergovernmental Panel on Climate Change.
1990. Climate Change: The IPCC Scientific Assessment, J. T.
Houghton, G. J. Jenkins, and J. J. Ephraums, eds. New York:
Cambridge University Press. Reprinted by permission of Cambridge
University Press.
|