中国による地球温暖化への影響
Bengang Li1,2, Thomas Gasser3,4, Philippe Ciais3
1Sino-French Institute for Earth System Science, Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China.
Nature
|March 18, 2016
まとめ
温室効果ガスや黒い炭素による温暖化効果と 硫酸エロゾールの冷却効果により,中国は世界的な放射能強制に10%の貢献をしている. 温室効果ガスの削減によってバランスをとらなければ 将来の空気質の改善が温暖化を加速する可能性があります
科学分野:
- 気候科学
- 大気化学
- 環境科学
背景:
- 地球規模の気候変動の緩和は 放射能強制への国の貢献を理解することに 依存しています
- 中国の急速な経済成長は排出量の増加につながりましたが,放射性強制への影響は不明でした.
- "共通だが差異のある責任"の原則は,個々の国の貢献を定量化することを必要とします.
研究 の 目的:
- 世界の放射能への影響を 定量化するためです
- 温室効果ガスの混合,短期的な気候変動,土地利用の変化による貢献を区別する.
- 空気質政策が将来の放射能強制に与える影響を予測する.
主な方法:
- 生物化学と気候モデルを組み合わせた
- 大気シミュレーションのための化学と輸送モデルを使用した.
- CO2,CH4,エアロゾール (硫酸塩,窒素,黒炭) による量化放射力,およびアルベドの変化.
主要な成果:
- 中国は,現在の世界の放射能強制力の10%±4%を占めています.
- ポジティブ (温暖化) フォースリングに12%±2%貢献する (温室効果ガス,ブラックカーボン).
- 負の (冷却) 強制 (硫酸塩,窒素エロゾール) に15%±6%貢献する.
結論:
- 中国の放射能は 地球規模の放射能強制に 大きく影響しています
- 空気の質のために二酸化硫黄を減らすことは 将来の温暖化を増加させるかもしれません
- 温暖化と冷却効果のバランスをとるには 短命の気候要因と 長期的な気候要因の両方を管理する必要があります
さらに関連する動画
関連する概念動画
Global Climate Change
29.6K
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.
29.6K
Microbes and Climate Change
15
Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
15
What is Climate?
21.3K
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.
21.3K
The Carbon Cycle
45.4K
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.
45.4K
Radiation: Applications
2.0K
The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
The average...
The average...
2.0K
Threats to Biodiversity
27.8K
There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
27.8K


