Английская Википедия:Airborne fraction
The airborne fraction is a scaling factor defined as the ratio of the annual increase in atmospheric [[CO2|Шаблон:Chem]] to the Шаблон:Chem emissions from human sources.[1] It represents the proportion of human emitted Шаблон:CO2 that remains in the atmosphere. Observations over the past six decades show that the airborne fraction has remained relatively stable at around 45%.[2] This indicates that the land and ocean's capacity to absorb CO2 has kept up with the rise in human CO2 emissions, despite the occurrence of notable interannual and sub-decadal variability, which is predominantly driven by the land's ability to absorb CO2. There is some evidence for a recent increase in airborne fraction, which would imply a faster increase in atmospheric Шаблон:Chem for a given rate of human fossil-fuel burning.[3] Changes in carbon sinks can affect the airborne fraction as well.
Discussion about the trend of airborne fraction
Anthropogenic CO2 that is released into the atmosphere is partitioned into three components: approximately 45% remains in the atmosphere (referred to as the airborne fraction), while about 24% and 31% are absorbed by the oceans (ocean sink) and terrestrial biosphere (land sink), respectively.[4] If the airborne fraction increases, this indicates that a smaller amount of the CO2 released by humans is being absorbed by land and ocean sinks, due to factors such as warming oceans or thawing permafrost. As a result, a greater proportion of anthropogenic emissions remains in the atmosphere, thereby accelerating the rate of climate change. This has implications for future projections of atmospheric CO2 levels, which must be adjusted to account for this trend.[5] The question of whether the airborne fraction is rising, remaining steady at approximately 45%, or declining remains a matter of debate. Resolving this question is critical for comprehending the global carbon cycle and has relevance for policymakers and the general public.
The quantity “airborne fraction” is termed by Charles David Keeling in 1973, and studies conducted in the 1970s and 1980s defined airborne fraction from cumulative carbon inventory changes as,[5]
<math>AF_{FF} = \frac{\frac{dC(t)}{dt}}{FF(t)}</math>
Or,
<math>AF_{FF+LU} = \frac{\frac{dC(t)}{dt}}{FF(t)+LU(t)}</math>
In which C is atmospheric carbon dioxide, t is time, FF is fossil-fuel emissions and LU is the emission to the atmosphere due to land use change.
At present, studies examining the trends in airborne fraction are producing contradictory outcomes, with emissions linked to land use and land cover change representing the most significant source of uncertainty. Some studies show that there is no statistical evidence of an increasing airborne fraction and calculated airborne fraction as,[6]
<math>AF = \frac{G_t}{E_{FF}+E_{LUC}}</math>
Where Gt is growth of atmospheric CO2 concentration, EFF is the fossil-fuel emissions flux, ELUC is the land use change emissions flux.
Another argument was presented that the airborne fraction of CO2 released by human activities, particularly through fossil-fuel emissions, cement production, and land-use changes, is on the rise.[7] Since 1959, the average CO2 airborne fraction has been 0.43, but it has shown an increase of approximately 0.2% per year over that period.[3]
On the other hand, the findings of another group suggest that the CO2 airborne fraction has declined by 0.014 ± 0.010 per decade since 1959.[8] This indicates that the combined land-ocean sink has expanded at a rate that is at least as rapid as anthropogenic emissions. The way they calculated the airborne fraction is:
<math>AF = \frac{E_{LULCC}+E_{FF}-S_O-S_L}{E_{LULCC}+E_{FF}}=1-SF</math>
Where, AF is airborne fraction and SF is sink fraction. ELULCC is the land use and land cover change emissions flux, EFF is the fossil-fuel emissions flux, and SO and SL are the ocean and land sinks, respectively.
The trend analyses of airborne fraction may be affected by external natural occurrences, such as the El Niño-Southern Oscillation (ENSO), volcanic eruptions, and other similar events.[9] It is possible that the methodologies used in these studies to analyze the trend of airborne fraction are not robust, and therefore, the conclusions drawn from them are not warranted.
See also
- Greenhouse gas
- Carbon dioxide in Earth's atmosphere
- Total Carbon Column Observing Network
- Atmospheric carbon cycle
References
- ↑ Forster, P, V Ramaswamy, P Artaxo, et al. (2007) Changes in Atmospheric Constituents and in Radiative Forcing. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [Solomon, S. et al. (eds.)]. Cambridge University Press, Cambridge, UK & New York, USA.[1]
- ↑ Шаблон:Cite journal
- ↑ 3,0 3,1 Шаблон:Cite journal
- ↑ Шаблон:Cite journal
- ↑ 5,0 5,1 Шаблон:Cite journal
- ↑ Шаблон:Cite journal
- ↑ Шаблон:Cite journal
- ↑ Шаблон:Cite journal
- ↑ Шаблон:Cite journal
