MadSci Network: Environment & Ecology |
The answer is in the abundance of the different atmospheric gases. Basically, the amount of oxygen in the atmosphere is much, much larger than carbon dioxide. In photosynthesis and respiration processes, about 11 molecules of O2 are exchanged for 10 molecules of CO2; the imbalance is covered by other chemical processes. The plant photosynthesis happening in North America results in a change in CO2 concentration of about 10 ppmv; that is, in units of molecules of CO2 per total molecules of air, the wintertime CO2 over North America is about 0.000010 higher than summertime. Since the concentration of CO2 in the atmosphere is about 0.000392, this is a relatively big change, about 2.5%, between summer and winter. However, the concentration of O2 in the atmosphere is roughly 0.2, so even though the seasonal change in O2 concentration is actually larger than CO2 (because of processes happening over the ocean), a seasonal change of +/-20 parts per million (0.000020) will change O2 concentrations by only 0.01%, which you could never detect. Running in the winter is probably easier because of the lower moisture in the air. This obviously only works in places where winter is relatively mild! There is lots of really good information about the carbon cycle and carbon dioxide available on the WWW (see for instance, http://en.wikipedia.or g/wiki/Keeling_Curve), but I had to go to a scholarly source to get the numbers for oxygen (Martin Heimann, "The Cycle of Atmospheric Molecular Oxygen and its Isotopes", in _Global Biogeochemical Cycles in the Climate System_, ed. Ernst-Detlef Schulze et al., Academic Press 2001).
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