Contribution of natural and anthropogenic emissions of CO2 and CH4 to the atmosphere from the territory of Russia to global climate change in the 21st century

S. Denisov, A. Eliseev, I. Mokhov
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引用次数: 1

Abstract

Obtained the estimates of the contribution of anthropogenic and natural GHG emissions into the atmosphere from the territory of Russia to global climate change under various scenarios of anthropogenic impact in the 21st century. Accounting for changes in climatic conditions can strongly influence the indicators of the impact of various greenhouse gas emissions on the climate system, especially at large time horizons. Moreover, depending on the planning horizon, the role of the natural fluxes of greenhouse gases into the atmosphere from terrestrial ecosystems may change. Currently, terrestrial ecosystems in the Russian regions affect global temperature in both directions: absorbing CO2 from the atmosphere contributes to slowing its growth, and emitting CH4 into the atmosphere accelerates warming. The net effect of the natural fluxes of these greenhouse gases from the Russian regions in modern conditions helps to slow down warming. This net effect is increasing in the first half of the 21st century, and after reaching a maximum (depending on the anthropogenic emission scenario) decreases by the end of the century under all the considered anthropogenic impact scenarios due to an increase in natural CH4 emissions and a decrease in CO2 absorption by terrestrial ecosystems.
俄罗斯境内自然和人为向大气排放的CO2和CH4对21世纪全球气候变化的贡献
获得了在21世纪各种人为影响情景下,俄罗斯境内人为和自然排放到大气中的温室气体对全球气候变化的贡献估算。考虑到气候条件的变化可以对各种温室气体排放对气候系统的影响的指标产生重大影响,特别是在大的时间范围内。此外,根据规划范围的不同,从陆地生态系统进入大气的温室气体自然通量的作用可能会发生变化。目前,俄罗斯地区的陆地生态系统对全球温度的影响是双向的:从大气中吸收二氧化碳有助于减缓其增长,而向大气中排放CH4则加速了变暖。在现代条件下,来自俄罗斯地区的这些温室气体的自然通量的净效应有助于减缓变暖。这一净效应在21世纪上半叶呈增加趋势,在所有考虑的人为影响情景下,由于自然CH4排放增加和陆地生态系统吸收二氧化碳减少,在达到最大值(取决于人为排放情景)后,到本世纪末将减少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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