由自然二氧化碳循环的人为增强驱动的未来海洋超
Ben I McNeil1,2, Tristan P Sasse1,3
1Climate Change Research Centre, University of New South Wales, Sydney, New South Wales, Australia.
Nature
|January 22, 2016
概括
由于二氧化碳 (CO2) 含量高, 海洋超气在2100年将增加十倍, 威胁海洋生物和渔业. 这种扩大二氧化碳循环对全球渔业的风险比预期早了几十年.
科学领域:
- 海洋学
- 海洋生物学
- 气候科学
背景情况:
- 海水中二氧化碳 (CO2) 度升高,被称为海洋超,会对海洋动物的神经系统,生理和行为产生负面影响.
- 准确预测海洋超需要了解每年海洋二氧化碳的变化,但全球观测数据很少.
研究的目的:
- 分析每月海洋二氧化碳度变化的全球模式.
- 在大气二氧化碳上升的情况下,研究海洋表面二氧化碳水平的年度循环.
- 为了预测海洋超的未来演变.
主要方法:
- 使用全球观测数据来确定月度二氧化碳度的变化.
- 分析了海洋表面二氧化碳的年度循环.
- 在未来预测中采用代表性度路径8.5 (RCP8.5) 场景.
主要成果:
- 根据RCP8.5情景,预计到2100年某些地区的海洋二氧化碳波动将增加十倍.
- 在增强的年度二氧化碳循环中确定了不同的全球模式.
- 预计大气中的二氧化碳含量达到650ppm, 到2100年可能会影响半个海洋表面.
结论:
- 扩大每年的二氧化碳循环在南洋,太平洋和北大西洋创造了"二氧化碳热点",使得渔业风险较早出现.
- 二氧化碳的非线性放大是由季节性二氧化碳动态和人为二氧化碳储存导致的海洋缓冲容量减少所驱动的.
- 在2100年之前, 海洋超级鱼将对全球渔业产生严重影响.
相关概念视频
The Carbon Cycle
45.5K
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.
45.5K
Global Climate Change
29.7K
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.
29.7K
The Sulfur Cycle
53.4K
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
53.4K
Microbes and Climate Change
46
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...
46
Carbon-dioxide Fixation
862
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...
862
The Phosphorus Cycle
44.9K
Unlike carbon, water, and nitrogen, phosphorus is not present in the atmosphere as a gas. Instead, most phosphorus in the ecosystem exists as compounds, such as phosphate ions (PO43-), found in soil, water, sediment and rocks. Phosphorus is often a limiting nutrient (i.e., in short supply). Consequently, phosphorus is added to most agricultural fertilizers, which can cause environmental problems related to runoff in aquatic ecosystems.
44.9K


