利用 CMIP6 模型集合评估俄罗斯地区大气中二氧化碳和甲烷的自然汇和源及其对 21 世纪气候变化的贡献

Pub Date : 2024-07-02 DOI:10.1134/s0001433824700142
S. N. Denisov, A. V. Eliseev, I. I. Mokhov
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引用次数: 0

摘要

摘要 利用国际 CMIP6 项目全球气候模型的模拟结果,分析了 21 世纪俄罗斯境内二氧化碳和甲烷向大气的自然通量。不同模型对俄罗斯地区二氧化碳自然通量的估算差异很大。21 世纪初的数值为-1 到 1 GtC/年。在 21 世纪,模型对通量估计的差异越来越大,到 21 世纪末,在人为影响最大的情景下,SSP5-8.5 的范围为-2.5 到 2.5 GtC/年。不同模型对俄罗斯境内向大气自然排放甲烷的估算也有很大差异。据估计,现代甲烷排放量在 10 到 35 兆吨碳氢化合物/年之间,21 世纪的增幅高达 300%。集合模型模拟显示了自然温室气体通量变化的总体趋势。大多数 CMIP6 模型的特点是陆地生态系统对二氧化碳的吸收达到最大值,并在 21 世纪末进一步减少,而所有模型和人为影响情景下排放到大气中的天然甲烷在整个 21 世纪都在增加。据估计,21 世纪俄罗斯境内自然 CO2 通量的累积温度潜力为-0.3 至 0.1 K,具体取决于人为影响情景,而自然 CH4 排放的加速变暖影响估计在 0.03 至 0.09 K 之间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Natural Sinks and Sources of CO2 and CH4 in the Atmosphere of Russian Regions and Their Contribution to Climate Change in the 21st Century Evaluated with the CMIP6 Model Ensemble

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Natural Sinks and Sources of CO2 and CH4 in the Atmosphere of Russian Regions and Their Contribution to Climate Change in the 21st Century Evaluated with the CMIP6 Model Ensemble

Abstract

The natural fluxes of CO2 and CH4 into the atmosphere from the territory of Russia in the 21st century have been analyzed using the results of simulations with the ensemble of global climate models of the international CMIP6 project. Estimates of natural CO2 fluxes in Russian regions differ greatly for different models. Their values for the beginning of the 21st century range from –1 to 1 GtC/year. In the 21st century, the differences in model estimates of fluxes are growing, and, at the end of the 21st century, in the scenario with the largest anthropogenic impacts, SSP5-8.5 range from –2.5 to 2.5 GtC/year. Estimates of natural methane emissions to the atmosphere from the territory of Russia also differ greatly for different models. Modern methane emissions are estimated in the range from 10 to 35 MtCH4/year, with an increase in the 21st century of up to 300%. Ensemble model simulations show general trends for changes in natural greenhouse gas fluxes. Most CMIP6 models are characterized by a maximum of CO2 uptake by terrestrial ecosystems and its further reduction by the end of the 21st century, while natural methane emissions to the atmosphere for all models and scenarios of anthropogenic impacts grow throughout the 21st century. The cumulative temperature potential of natural CO2 fluxes on the territory of Russia in the 21st century is estimated, depending on the scenario of anthropogenic impacts, to be from –0.3 to 0.1 K, and the accelerating warming impact of natural CH4 emissions is estimated in the range of 0.03–0.09 K.

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