Multiple Scenarios Simulation of Global Ecological Footprint Based on Empirical Mode Decomposition Method

L. Xiang, Chengzhong Chen
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Abstract

A nonlinear dynamic simulative model has been discussed with variable cycles of entire world per capita ecological footprint taken from 1961 to 2003. The model was further classified and decomposed and extracted by the empirical mode decomposition (EMD) method. To deal with the problems proposed in the Living Planet Report 2006, three ecological footprint scenarios are presented. Simulative numerical values of the three global per capita (GPC) ecological footprint scenarios are also analyzed based on the simulative model. The results show that: 1) The clear varying cycle of global per capita EF growth is 4.6 years, 9.5 years, 19.5 years and 41 years over the last 42 years; 2) According to the business-as-usual scenario, if the global per capita increases positively with the constant growth, it is expected that GPC EF would be 3.262 gha in 2050. Assuming global per capita biocapacity (BC) to be 1.236 gha, global per capita ecological deficit (ED) would increase from 0.4 gha in 2003 to 2.026 gha in 2050; 3) The slow-shift scenario shows global per capita EF would decrease from 2.23 gha in 2003 to 1.619 gha in 2080 and 1.406 gha in 2100, if the negative annual change rate of it is 0.447 percent. Global per capita ED would decrease from 0.4 gha in 2003 to 0.222 gha in 2080 and 0.038 gha in 2100, if global per capita BC is 1.397 gha; 4) The rapid-reduction scenario depicts global per capita EF would decrease to 1.414 gha in 2050, if the negative annual change rate is 0.842% from 2003 to 2050. Assuming global per capita BC to be 1.461 gha, global per capita ecological reserve (ER) would be 0.047 gha, and overshoot would be eliminated in 2050. Global per capita EF would decrease to 1.054 gha in 2100, if the negative annual change rate is 0.438% from 2050 to 2100. Assuming global per capita BC to be 1.474 gha, GPC ER would be 0.420 gha. Then, wild species of the planet will be allocated nearly 28.5% of the planet’s biological productivity, which coincides with the results of Living Planet Report 2006.
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基于经验模态分解方法的全球生态足迹多情景模拟
本文讨论了1961 ~ 2003年全球人均生态足迹变周期的非线性动态模拟模型。采用经验模态分解(EMD)方法对模型进行进一步分类、分解和提取。为了解决《地球生命力报告2006》中提出的问题,本文提出了三种生态足迹设想。在此基础上,对三种全球人均生态足迹情景的模拟数值进行了分析。结果表明:①近42年来,全球人均生态环境增长率的变化周期分别为4.6年、9.5年、19.5年和41年;2)在不变情景下,如果全球人均持续增长,预计2050年GPC EF为3.262 gha。假设全球人均生物承载力(BC)为1.236 gha,全球人均生态赤字(ED)将从2003年的0.4 gha增加到2050年的2.026 gha;3)在缓慢变化情景下,全球人均温室气体排放量将从2003年的2.23 gha下降到2080年的1.619 gha和2100年的1.406 gha,其负年变化率为0.447%。如果全球人均BC为1.397 gha,全球人均ED将从2003年的0.4 gha下降到2080年的0.222 gha和2100年的0.038 gha;(4)在快速减少情景下,如果2003 - 2050年的负年变化率为0.842%,2050年全球人均EF将减少到1.414 gha。假设全球人均BC为1.461 gha,则全球人均生态储备(ER)为0.047 gha,到2050年可消除超量。如果2050 - 2100年的负年变化率为0.438%,到2100年全球人均温室气体排放量将减少到1.054 gha。假设全球人均BC为1.474 gha, GPC ER将为0.420 gha。然后,地球上的野生物种将被分配近28.5%的地球生物生产力,这与2006年地球生命力报告的结果一致。
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