北美的一个大型陆地碳汇,由大气和海洋二氧化碳数据和模型暗示
1S. Fan and J. Sarmiento, Atmospheric and Oceanic Sciences Program, Princeton University, Princeton, NJ 08544, USA. M. Gloor and S. Pacala, Department of Ecology and Evolutionary Biology, Princeton University, Princeton, NJ 08542, USA. J. Mahlm.
概括
全球陆地生态系统在1988-1992年间每年吸收1.0至2.2百克的碳. 北美显示显著的二氧化碳吸收,而欧亚和非洲的净交换最小.
科学领域:
- 地球系统科学 地球系统科学
- 大气化学 大气化学
- 生态生态学 生态生态学
背景情况:
- 大气中的二氧化碳 (CO2) 度在全球范围内一直在上升.
- 了解陆地碳汇对于气候变化建模至关重要.
研究的目的:
- 量化全球陆地二氧化碳的吸收.
- 为了确定这个陆地碳汇的空间分布.
主要方法:
- 利用了1988-1992年的大气二氧化碳数据.
- 采用了两个大气运输模型.
- 包括化石燃料排放和海洋二氧化碳吸收的估计.
主要成果:
- 全球陆地吸收量估计为每年1.0至2.2百克的碳 (Pg C年-1).
- 北美地区的显著摄入量为1.7 +/- 0.5 Pg C年-1.
- 欧亚-北非地区的吸收率较低 (0.1 +/- 0.6 Pg C年-1),其他陆地地区是净来源 (0.2 +/- 0.9 Pg C年-1).
结论:
- 陆地生态系统在减轻大气二氧化碳的增加方面发挥着至关重要的作用.
- 在陆地碳汇的有效性方面存在显著的区域差异.
相关概念视频
What are Biogeochemical Cycles?
The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
The Carbon Cycle
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.
The Nitrogen Cycle
Nitrogen atoms, present in all proteins and DNA, are recycled between abiotic and biotic components of the ecosystem. However, the primary form of nitrogen on Earth is nitrogen gas, which cannot be used by most animals and plants. Thus, nitrogen gas must first be converted into a usable form by nitrogen-fixing bacteria before it can be cycled through other living organisms. The use of nitrogen-containing fertilizers and animal waste products in human agriculture has greatly influenced the...
Global Climate Change
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.
Microbes and the Carbon Cycle
The carbon cycle is a fundamental Earth process involving the transfer of carbon among the biosphere, lithosphere, atmosphere, and hydrosphere. It plays a critical role in regulating the planet’s climate and supporting life by cycling carbon through various chemical forms and reservoirs. Carbon primarily circulates as carbon dioxide (CO₂), representing its oxidized form, while reduced forms such as methane (CH₄) and organic compounds also play essential roles.Microbial activity is central to...
Microbes and Climate Change
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...


