大气中的二氧化碳度在最后一个冰川结束时
E Monnin1, A Indermühle, A Dällenbach
1Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland.
概括
大气中的二氧化碳 (CO2) 水平在最后一次降冰期间在6000年内上升了76ppm. 南洋和北半球/热带过程都影响了这种显著的二氧化碳增加.
科学领域:
- 古气候学 古气候学
- 冰核科学 冰核科学
- 气候变化研究 气候变化研究
背景情况:
- 了解过去的气候转型对于预测未来的气候变化至关重要.
- 大气中的二氧化碳 (CO2) 和甲 (CH4) 是影响全球气候的关键温室气体.
- 冰芯为大气组成和温度提供了宝贵的长期记录.
研究的目的:
- 为了重建大气中的二氧化碳度在最后的冰川最大到全新世过渡期间.
- 研究二氧化碳变化,南极温度和甲变化之间的关系.
- 为了确定驱动CO2在脱冰过程中增加的关键区域和过程.
主要方法:
- 来自南极洲康科迪亚圆顶冰芯的分析. 南极洲.
- 从冰芯记录中测量大气中的二氧化碳 (CO2) 度.
- 对二氧化碳趋势与南极温度数据和大气中甲度的比较.
主要成果:
- 在6000年间,大气中的二氧化碳量显著增加了76个百万分之一的体积 (ppmv).
- 二氧化碳的增加发生在四个不同的间隔,与南极温度变化密切相关.
- 二氧化碳和甲度变化之间的相似性表明来自热带和北半球来源的贡献.
结论:
- 南大洋在脱冰过程中的二氧化碳增加中发挥了重要作用.
- 热带和北半球的过程是主要的甲来源,也大大影响了大气中的CO2.
- 降冰涉及不同地球系统之间的复杂相互作用,影响温室气体水平.
更多相关视频
相关概念视频
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 Sulfur Cycle
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...
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.
Phase Transitions: Sublimation and Deposition
Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
Phase Diagrams
A phase diagram combines plots of pressure versus temperature for the liquid-gas, solid-liquid, and solid-gas phase-transition equilibria of a substance. These diagrams indicate the physical states that exist under specific conditions of pressure and temperature and also provide the pressure dependence of the phase-transition temperatures (melting points, sublimation points, boiling points). Regions or areas labeled solid, liquid, and gas represent single phases, while lines or curves represent...
Carbon Dioxide Transport in the Blood
Carbon dioxide (CO2) transport in the blood is critical to human physiology. On average, our body cells produce around 200 mL of CO2 per minute, precisely the quantity expelled by the lungs. This process involves the transportation of CO2 from the tissue cells to the lungs in three primary forms.
Forms of CO2 Transport
1. Dissolved in plasma: A small percentage (7-10%) of CO2 is transported and dissolved directly in the plasma.
2. Carbaminohemoglobin: Just over 20% of CO2 is chemically bound to...
Forms of CO2 Transport
1. Dissolved in plasma: A small percentage (7-10%) of CO2 is transported and dissolved directly in the plasma.
2. Carbaminohemoglobin: Just over 20% of CO2 is chemically bound to...


