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Methane is emitted during the production and transport of coal, natural gas, and oil. Methane emissions also result from livestock and other agricultural practices and by the decay of organic waste in municipal solid waste landfills. The CH4 profile as a greenhouse gas (GHG) is shown below with other GHG’s and their warming potential, atmospheric lifetime, molecular weight and radiative forcing. Note that a full GHG budget would include measurements for all of the gases listed, however, rarely are such full budgets measured in practice. PαC intends to increase the number of GHG’s directly measured by the System of Systems network resulting in a multi-gas GHG emissions measurement and reduction approach.
Houweling, Sander, Peter Bergamaschi, Frederic Chevallier, Martin Heimann, Thomas Kaminski, Maarten Krol, Anna M. Michalak, and Prabir Patra. “Global inverse modeling of CH 4 sources and sinks: an overview of methods.” Atmospheric Chemistry and Physics 17, no. 1 (2017): 235-256.
Saunois, Marielle, Philippe Bousquet, Benjamin Poulter, Anna Peregon, Philippe Ciais, Josep G. Canadell, Edward J. Dlugokencky et al. “Variability and quasi-decadal changes in the methane budget over the period 2000-2012.” Atmospheric Chemistry and Physics Discussions (2017): 1-39.
CO2 is the basis of life on Earth. While CO2 courses through the planetary fabric of earth, water, plants and the atmosphere, it also runs through our lives as the defining anthropogenic imprint on the world humanity has created. Small amounts of CO2 added to the atmosphere since the industrial revolution have enhanced surface warming and the dynamics of the Earth system. Small changes in the climate system can wield a host of disruptions to the lifeways of society involving food and water availability, energy production and our economic systems. The CO2 profile as a greenhouse gas (GHG) is shown below with other GHG’s and their warming potential, atmospheric lifetime, molecular weight and radiative forcing. Note that a full GHG budget would include measurements for all of the gases listed, however, rarely are such full budgets measured in practice. PαC intends to increase the number of GHG’s directly measured by the System of Systems network resulting in a multi-gas GHG emissions measurement and reduction approach.
Campbell, J. E., J. A. Berry, U. Seibt, Steven J. Smith, S. A. Montzka, T. Launois, S. Belviso, L. Bopp, and M. Laine. “Large historical growth in global terrestrial gross primary production.” Nature 544, no. 7648 (2017): 84-87.
Lovenduski, Nicole S., and Gordon B. Bonan. “Reducing uncertainty in projections of terrestrial carbon uptake.” Environmental Research Letters 12, no. 4 (2017): 044020.
Ussiri, David AN, and Rattan Lal. “Introduction to Global Carbon Cycling: An Overview of the Global Carbon Cycle.” In Carbon Sequestration for Climate Change Mitigation and Adaptation, pp. 61-76. Springer International Publishing, 2017.
When conservation of forests are tied to protection of endangered species forest destruction is limited. As a consequence, efflux of CO2 to the atmosphere from deforestation and soil disturbances are retained. The same avoidance mechanism is provided by species conservation as for Indigenous Peoples. The sealed Biosphere Box signifies the retention of ecosystem carbon by conserving and protecting areas for Gorilla habitat.
Imani, Gérard, Faustin Boyemba, Simon Lewis, Nsharwasi Léon Nabahungu, Kim Calders, Louis Zapfack, Bernard Riera, Clarisse Balegamire, and Aida Cuni-Sanchez. “Height-diameter allometry and above ground biomass in tropical montane forests: Insights from the Albertine Rift in Africa.” PloS one12, no. 6 (2017): e0179653.
Sheil, Douglas, Brenton Ladd, Lucas CR Silva, Shawn W. Laffan, and Miriam Van Heist. “How are soil carbon and tropica