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相关概念视频

Global Climate Change01:50

Global Climate Change

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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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Trophic level transfer efficiency (TLTE) is a measure of the total energy transfer from one trophic level to the next. Due to extensive energy loss as metabolic heat, an average of only 10% of the original energy obtained is passed on to the next level. This pattern of energy loss severely limits the possible number of trophic levels in a food chain.
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An ecological disturbance is a temporary disruption in the environment resulting from abiotic, biotic, or anthropogenic factors, causing a pronounced change in an ecosystem. The impact of an ecological disturbance, which can depend on its intensity, frequency, and spatial distribution, plays a significant role in shaping the species diversity within the ecosystem.
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During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance. Over a...
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在全球范围内,海拔升高改变了生态系统的特性.

Jordan R Mayor1, Nathan J Sanders2,3, Aimée T Classen2,3

  • 1Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, Umeå 90187, Sweden.

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温度随着海拔上升而下降,影响植物营养和土壤. 这些树林生态变化表明未来的变暖可能会破坏全球的山区生态系统功能.

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科学领域:

  • 生态学
  • 生物地质化学
  • 气候科学

背景情况:

  • 温度是影响生物多样性和生态系统边界的关键因素.
  • 对于了解对气候变化的生态反应至关重要.
  • 从森林到高山原的过渡是一个独特的生态边界.

研究的目的:

  • 调查地面和地下生态系统对高度温度变化的反应的全球一致性.
  • 解开温度对植物群落和土壤特性的直接和间接影响.
  • 评估全球七个温带地区的树林生态特征.

主要方法:

  • 在高度梯度上评估树叶营养度.
  • 量化地面层植物和的体质测量.
  • 分析了土壤中的有机物质含量,碳比和微生物特性.

主要成果:

  • 气温下降并没有改变树叶的营养.
  • 地层植物随着海拔的提高而减少,导致与的比率趋同.
  • 高度驱动的营养变化与土壤有机物和微生物性质的改变相关.

结论:

  • 温度直接影响地面层的植物度,并间接影响树林边界的土壤特性.
  • 未来的气候变暖可能会破坏山区生态系统的功能,特别是如果植物群体的重组速度比树林的增长速度快.