On the critical mass of greenhouse gas
DOI:
https://doi.org/10.24028/gzh.0203-3100.v40i1.2018.124016Keywords:
greenhouse gas, positive feedback, temperature rise, bifurcation transitionAbstract
In recent years, changes in the Earth’s climate have raised concern all around the globe. Climatologists have been drawing connections between global warming and a growing number of natural disasters, unexpected temperature fluctuations in some regions of the world and a number of other climatic aberrations. Within the scientific community, the opinions as to the nature and mechanism of the Earth’s climate change have split. Some contend that since the beginning of the industrial revolution, the carbon dioxide levels in the air have been steadily rising due to human production activities. Along with other gases, carbon dioxide has been inculpated for the greenhouse effect. In connection with this, a number of recent international conferences have adopted resolutions to reduce carbon dioxide emissions into the atmosphere. Another group of climatologists bases its findings on observations of solar activity, arguing that global warming is caused by a recurring spike in solar activity, with the current increase due to end soon, potentially giving way to a new ice age down the road. In the following work, we put forth yet another hypothesis regarding global warming. The influence of four main positive feedback loops caused by the secondary emission of water vapor, ÑÎ2, ÑÎ4, and decreased albedo on the earth climate system is shown on the basis of the general theory of feedback. If the present level of primary anthropogenic emissions of greenhouse gas (GhG) keeps, the total mass of atmospheric greenhouse gas can run up to such a critical value that the mentioned feedbacks, which give rise to self-amplification of the greenhouse effect, can cause the bifurcation transition of the climate system to the state of self-heating tending to the unlimited rise of mean temperature of the earth surface.
References
Bode H. W., 1945. Network analysis and feedback amplifier design. New York: D. Van Nostrand Co.
Klimchuk E. F., Tarasov V. F., 2005. On one model of a greenhouse effect. Geofizicheskiy zhurnal 27(5), 906—910 (in Russian).
Lashof D. A., DeAngelo B. J., Saleska S. R., Harte J., 1997. Terrestrial Ecosystem Feedbacks to clobal climate change. Annu. Rev. Energy. Environ. 22, 75—118.
MacDougall A. H., Knutti R., 2016. Enhancement of non-CO 2 radiative forcing via intensified carbon cycle feedbacks. Geophys. Res. Lett. 43, 5833—5840. doi: 10.1002/2016GL068964.
MacDougall A. H., Zickfeld K., Knutti R., Matthews H. D., 2015. Sensitivity of carbon budgets to permafrost carbon feedbacks, non-CO 2 forcings, and negative emissions. Environ. Res. Lett. 10(12). doi: 10.1088/1748-9326/10/12/125003.
Petit J.-R., Jouzel J., Raynaud D., Barkov N. I., Barnola J.-M., Basile I., Bender M., Chappellaz J., Davis M., Delaygue G., Delmotte M., Kotlyakov V. M., Legrand M., Lipenkov V., Lorius C., Pepin L., Ritz C., Saltzman E., Stievenard M., 1999. Climate and atmospheric history of the past 420,000 years from the Vostok ice core Antarctica. Nature 399, 429—436. doi:10.1038/20859.
Plattner R., Knutti R., Friedlingtein P., 2009. Irreversible climate change due to carbon dioxide emissions. Proc. of the National Academy of Sciences 106, 1704—1709. doi: 10.1073/pnas.0812721106.
Raisbeck G., 1954. A definition of passive linear net-works in terms of time and energy. J. Appl. Phys. 25, 1510—1514.
Rugenstein M. A. A., Caldeira K., Knutti R., 2016. Dependence of global radiative feedbacks on evolving patterns of surface heat fluxes. Geophys. Res. Lett. 43, 9877—9885. doi: 10.1002/2016GL070 907.
Schaller N., Sedláèek J., Knutti R., 2014. The asymmetry of the climate system’s response to solar forcing changes and its implications for geoengineering scenarios. J. Geophys. Res. 119, 5171—5184. doi: 10.1002/2013JD021258.
Scheffer M., Brovkin V., Cox P., 2006. Positive feedback between global warming and atmospheric ÑÎ2 concentration inferred from past climate change. Geophys. Res. Lett. 33, L10702, doi: 10.1029/2005GL025044.
Torn M. S., Harte J., 2006. Missing feedbacks, asymmetric uncertainties, and the underestimation of future warning. Geophys. Res. Lett. 33, L10703. doi:10.1029/2005GLO25540.
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 2020 Geofizicheskiy Zhurnal
This work is licensed under a Creative Commons Attribution 4.0 International License.
Authors who publish with this journal agree to the following terms:
1. Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.
2. Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.
3. Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access).