International Journal of Geosciences

Volume 7, Issue 10 (October 2016)

ISSN Print: 2156-8359   ISSN Online: 2156-8367

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Oceans, Ice & Snow and CO2 Rise, Swing and Seasonal Fluctuation

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DOI: 10.4236/ijg.2016.710092    2,617 Downloads   3,997 Views  Citations

ABSTRACT

Carbon dioxide rise, swing and spread (seasonal fluctuations) are addressed in this study. Actual CO2 concentrations were used rather than dry values. The dry values are artificially higher because water vapor must be removed in order for the NDIR instrument to work and is not factored back into the reported numbers. Articles addressing these observations express opinions that are divergent and often conflicting. This investigation resolves many of those inconsistencies. The data were obtained from many measuring stations at various latitudes since 1972 and then graphical compared to changes in sea temperatures, fossil fuel emissions, humidity, and seasonal ice and snow changes. In analyzing the data, various parameters were addressed including: variability, R squared curve values, correlations between curves, residence times, absorption percentages, and Troposphere effects. Mass balance calculations were also made to corroborate viability. The CO2 “rise” over a 33-year period from a slight ocean temperature increase (0.7°F) contributed 2.3 percent of the total rise while fossil fuel emissions contributed 1.5 percent. The overwhelming majority (60 ppmv, 96%+) was caused by other factors including ocean and land biology as well potential errors in fundamental hypotheses. With respect to “spread” (seasonal CO2 fluctuations) at the Polar Circles, graphical analysis with high correlations supported by mass balance calculations confirm that ice and snow are the primary cause and explain why the concentrations are the highest at these cold locations. The global variations in “swing” remain uncertain.

Share and Cite:

Nelson, M. and Nelson, D. (2016) Oceans, Ice & Snow and CO2 Rise, Swing and Seasonal Fluctuation. International Journal of Geosciences, 7, 1232-1282. doi: 10.4236/ijg.2016.710092.

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