厄尔尼诺/南方振荡和热带太平洋气候在过去的千年
Kim M Cobb1, Christopher D Charles, Hai Cheng
1Scripps Institution of Oceanography, University of California-San Diego, La Jolla, California 92093, USA. kcobb@gps.caltech.edu
Nature
|July 18, 2003
概括
了解过去的厄尔尼诺/南方振荡 (ENSO) 变化对于气候变化评估至关重要. 珊瑚记录显示,ENSO活动在17世纪中叶达到顶峰,这表明内部系统动态驱动了它的大部分变化.
科学领域:
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
背景情况:
- 未来的气候变化评估取决于对自然气候变化的理解.
- 厄尔尼诺/南方振荡 (ENSO) 是热带太平洋气候变化的关键驱动因素.
研究的目的:
- 为了重建过去1100年的热带太平洋气候变化.
- 分析厄尔尼诺/南方振荡 (ENSO) 行为及其与平均气候条件的关系.
主要方法:
- 从帕尔米拉岛的化石-珊瑚氧气同位素记录一起拼接.
- 分析热带太平洋气候变化的30-150年窗口.
主要成果:
- 中部热带太平洋气候从凉爽/干燥 (十世纪) 转变为温暖/潮湿 (二十世纪).
- 观察到广泛的ENSO行为范围,与平均气候关系差.
- 最强烈的ENSO活动发生在17世纪中叶.
结论:
- 在过去的千年里,大部分的厄尔尼诺/南方振荡 (ENSO) 变化可能来自ENSO系统内部动态.
- 珊瑚同位素记录为过去的气候变化和ENSO行为提供了宝贵的见解.
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.
What is Climate?
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.
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.
Precipitation Processes
The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
Precipitation and Co-precipitation
Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
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...


