观测到的地方生产的碳分离不足以实现到2050年的净零目标
Maria Zioga1,2,3, Maximilian Kotz1, Anders Levermann1,2
1Research Department of Complexity Science, Potsdam Institute for Climate Impact Research, Potsdam 14473, Germany.
概括
地方气候行动是实现净零排放的关键. 虽然一些地区在将经济增长与碳排放脱方面取得了进展,但目前的速度不足以实现到2050年的全球气候目标.
科学领域:
- 环境科学 环境科学
- 气候变化经济学 气候变化经济学
- 区域政策分析 区域政策分析
背景情况:
- 从历史上看,经济增长与碳排放相关,推动了气候变化.
- 稳定全球气温需要实现净零碳排放.
- 目前的减排率和经济脱不足以实现全球气候目标.
研究的目的:
- 评估地方气候行动在将经济增长与碳排放脱方面的有效性.
- 为了估计三十年来全球不同地区的脱率和二氧化碳排放强度.
- 确定影响在地方一级成功脱的因素.
主要方法:
- 分析报告的经济产出和30年来1500多个国家以下地区 (覆盖全球排放量的85%) 的基于生产的排放数据.
- 脱率和二氧化碳排放强度的估计.
- 基于收入,历史碳强度,地方气候支出和国家政策框架 (例如,经合组织,欧盟) 的脱率的比较分析.
主要成果:
- 30%的分析区域已经实现了经济增长与碳排放的完全脱.
- 高收入和历史上碳密集型地区的脱率更高,排放强度下降.
- 经合组织国家气候支出增加的次国家区域和实施气候政策的欧盟地区的脱率较高.
- 在国家边界内,脱率的变化比在国家边界之间更大,特别是在治理较弱的国家.
- 按照目前的速度,预计到2050年,不到一半的亚国家级地区将达到净零排放.
结论:
- 地方气候政策有效地推动了经济与碳排放的脱.
- 在分离进展方面存在显著的区域差异,需要量身定制的分国家级战略.
- 加快努力和政策实施对于在所需的时间框架内实现全球净零目标至关重要.
相关概念视频
The Carbon Cycle
37.1K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
37.1K
Global Climate Change
24.2K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
24.2K
Carbon-dioxide Fixation
1
Carbon dioxide fixation in prokaryotes enables the assimilation of inorganic carbon into organic molecules, supporting biosynthetic pathways, sustaining ecosystems, and contributing to the global carbon cycle. It also has industrial applications in carbon capture and bioproduct synthesis. Autotrophic organisms rely on this process to utilize CO₂ as a carbon source in diverse environments.The Calvin CycleThe Calvin cycle is the most widespread carbon fixation mechanism, primarily used by...
1
Primary Production
23.6K
The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
23.6K
¹³C NMR: ¹H–¹³C Decoupling
1.0K
The probability of having two carbon-13 atoms next to each other is negligible because of the low natural abundance of carbon-13. Consequently, peak splitting due to carbon-carbon spin-spin coupling is not observed in spectra. However, protons up to three sigma bonds away split the carbon signal according to the n+1 rule, resulting in complicated spectra.
A broadband decoupling technique is used to simplify these complex, sometimes overlapping, signals. Broadband decoupling relies on a...
A broadband decoupling technique is used to simplify these complex, sometimes overlapping, signals. Broadband decoupling relies on a...
1.0K
What is Climate?
18.4K
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
18.4K


