Buddhist Vegetarianism Views on Equivalent Reduction of Greenhouse Gas Emissions in China from 2017 to 2027

2019 ◽  
Vol 23 (3) ◽  
pp. 254-274
Author(s):  
Ampere A. Tseng

AbstractThe impact of Buddhist vegetarianism views on the equivalent reduction of greenhouse gas emissions (GHGE s) is evaluated. The vegetarianism views from three major Buddhist schools in China are first presented, since different views on vegetarianism can dictate the assessment of the equivalent of GHGE reduction. The populations of Chinese Buddhists in these three Buddhist schools are then estimated. A correlation formula is used to evaluate the equivalent GHGE reductions attributed to the vegan and vegetarian populations in the Chinese Buddhists from 2017 to 2027. The reduction results enable us to conclude that Chinese Buddhists with vegan or vegetarian diets account for the equivalent GHGE reduction of 54.560 MtCO2e in 2017 and 60.927 MtCO2e in 2027 with an average annual growth rate of 1.11 %. The reductions of 54.560 and 60.927 MtCO2e equal to 11.66 % and 13.02 % of the total GHGE s from the United Kingdom in 2016, respectively.

2008 ◽  
Vol 2008 (6) ◽  
pp. 783-792 ◽  
Author(s):  
Patricia Scanlan ◽  
Holly Elmendorf ◽  
Hari Santha ◽  
James Rowan

2006 ◽  
Vol 19 (13) ◽  
pp. 3055-3069 ◽  
Author(s):  
Peter A. Stott ◽  
John F. B. Mitchell ◽  
Myles R. Allen ◽  
Thomas L. Delworth ◽  
Jonathan M. Gregory ◽  
...  

Abstract This paper investigates the impact of aerosol forcing uncertainty on the robustness of estimates of the twentieth-century warming attributable to anthropogenic greenhouse gas emissions. Attribution analyses on three coupled climate models with very different sensitivities and aerosol forcing are carried out. The Third Hadley Centre Coupled Ocean–Atmosphere GCM (HadCM3), Parallel Climate Model (PCM), and GFDL R30 models all provide good simulations of twentieth-century global mean temperature changes when they include both anthropogenic and natural forcings. Such good agreement could result from a fortuitous cancellation of errors, for example, by balancing too much (or too little) greenhouse warming by too much (or too little) aerosol cooling. Despite a very large uncertainty for estimates of the possible range of sulfate aerosol forcing obtained from measurement campaigns, results show that the spatial and temporal nature of observed twentieth-century temperature change constrains the component of past warming attributable to anthropogenic greenhouse gases to be significantly greater (at the 5% level) than the observed warming over the twentieth century. The cooling effects of aerosols are detected in all three models. Both spatial and temporal aspects of observed temperature change are responsible for constraining the relative roles of greenhouse warming and sulfate cooling over the twentieth century. This is because there are distinctive temporal structures in differential warming rates between the hemispheres, between land and ocean, and between mid- and low latitudes. As a result, consistent estimates of warming attributable to greenhouse gas emissions are obtained from all three models, and predictions are relatively robust to the use of more or less sensitive models. The transient climate response following a 1% yr−1 increase in CO2 is estimated to lie between 2.2 and 4 K century−1 (5–95 percentiles).


GCB Bioenergy ◽  
2016 ◽  
Vol 9 (3) ◽  
pp. 627-644 ◽  
Author(s):  
Mark Richards ◽  
Mark Pogson ◽  
Marta Dondini ◽  
Edward O. Jones ◽  
Astley Hastings ◽  
...  

2022 ◽  
Vol 37 ◽  
Author(s):  
Christopher M. Wade ◽  
Justin S. Baker ◽  
Jason P. H. Jones ◽  
Kemen G. Austin ◽  
Yongxia Cai ◽  
...  

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