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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.
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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.
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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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A CO2 Concentration Gradient Facility for Testing CO2 Enrichment and Soil Effects on Grassland Ecosystem Function
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全球植被产量可能会在本世纪减少,原因是大气干燥程度上升.

Shangrong Lin1, Xiuzhi Chen2, Jiangzhou Xia3

  • 1Guangdong Province Data Center of Terrestrial and Marine Ecosystems Carbon Cycle, School of Geography and Planning, Sun Yat-sen University, Guangzhou, China.

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此摘要是机器生成的。

大气中二氧化碳 (CO2) 的增加可能会促进植物生长,但气候变暖引起的干旱将抵消这种效应. 全球植被产量 (GPP) 预计将在本世纪中叶达到峰值,然后由于大气干燥增加而下降.

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科学领域:

  • 地球系统科学 地球系统科学
  • 气候变化研究 气候变化研究
  • 生态生态学 生态生态学

背景情况:

  • 以前的地球系统模型预测大气中二氧化碳 (CO2) 的增加将通过二氧化碳受精效应刺激全球植被生产.
  • 这种受精效应增强了光合作用和植物生长.

研究的目的:

  • 为了研究气候变暖带来的大气干旱如何影响全球植被产量.
  • 在不断变化的气候条件下,预测未来的全球植被总初级产量 (GPP).

主要方法:

  • 利用了来自全球-协变点的测量结果.
  • 采用基于过程的模型进行预测.
  • 分析了CO2,甲 (CH4) 和氧化 (N2O) 对GPP的影响.

主要成果:

  • 全球植被 GPP 预计将在21世纪中叶达到峰值,随后下降.
  • 与当前水平相比,GPP的峰值增加估计仅为5.4 ± 0.5%.
  • 大气干燥程度的增加显著抵消了二氧化碳受精效应,特别是在热带地区.
  • 非二氧化碳的温室气体 (CH4和N2O) 导致气候变暖和干旱,对GPP产生负面影响.

结论:

  • 气候变暖引起的大气干旱大大减少了陆地植被的生长.
  • 由于这些干燥效应,陆地碳汇在未来可能会受到限制.
  • 未来的植被生产力受到水资源的限制,而不仅仅是二氧化碳水平.