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相关概念视频

Global Climate Change01:50

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.
The Carbon Cycle01:14

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?01:16

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.
Microbes and Climate Change01:27

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...
What is Weather?01:07

What is Weather?

Overview
Threats to Biodiversity01:50

Threats to Biodiversity

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...

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相关实验视频

Updated: May 8, 2026

Simulating Temperature in a Soil Incubation Experiment
08:39

Simulating Temperature in a Soil Incubation Experiment

Published on: October 28, 2022

极端气候现象和碳循环

Markus Reichstein1, Michael Bahn, Philippe Ciais

  • 1Max Planck Institute for Biogeochemistry, 07745 Jena, Germany. markus.reichstein@bgc-jena.mpg.de

Nature
|August 20, 2013
PubMed
概括

干旱等极端气候现象可以减少生态系统的碳储量,可能抵消陆地碳吸收增加. 这项研究探讨了这些对全球碳循环的影响.

更多相关视频

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
07:32

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.

Published on: June 4, 2021

相关实验视频

Last Updated: May 8, 2026

Simulating Temperature in a Soil Incubation Experiment
08:39

Simulating Temperature in a Soil Incubation Experiment

Published on: October 28, 2022

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
07:32

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.

Published on: June 4, 2021

科学领域:

  • 地球系统科学 地球系统科学
  • 生态生态学 生态生态学
  • 气候科学 气候科学

背景情况:

  • 陆地生物圈在全球碳循环中起着至关重要的作用.
  • 预计环境变化将增加全球陆地碳吸收.
  • 极端气候可能会对区域生态系统的碳储量产生负面影响.

研究的目的:

  • 研究极端气候对陆地碳循环的机制和影响.
  • 提出改善对极端气候对陆地碳预算影响的理解方法.
  • 评估极端气候对全球碳平衡的未来影响.

主要方法:

  • 对气候极端和陆地碳循环现有文献的审查.
  • 分析与生态系统反应相关的观测数据和气候模型.
  • 在极端事件期间推动碳库存变化的机制的合成.

主要成果:

  • 干旱和风暴等极端气候现象可能会导致区域生态系统碳库存大幅减少.
  • 这些减少有可能抵消全球陆地碳吸收预期的增加.
  • 陆地碳预算对气候极端事件的频率和强度非常敏感.

结论:

  • 了解气候极端的影响对于准确的气候变化预测至关重要.
  • 需要进一步的研究来完善在不断变化的气候条件下对陆地碳循环的模型和预测.
  • 缓解和适应战略必须考虑极端气候对自然碳汇的破坏性影响.