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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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What is Climate?01:16

What is Climate?

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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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Responses to Heat and Cold Stress02:45

Responses to Heat and Cold Stress

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Every organism has an optimum temperature range within which healthy growth and physiological functioning can occur. At the ends of this range, there will be a minimum and maximum temperature that interrupt biological processes.
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Threats to Biodiversity01:50

Threats to Biodiversity

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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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Adaptations that Reduce Water Loss01:57

Adaptations that Reduce Water Loss

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Though evaporation from plant leaves drives transpiration, it also results in loss of water. Because water is critical for photosynthetic reactions and other cellular processes, evolutionary pressures on plants in different environments have driven the acquisition of adaptations that reduce water loss.
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Radiation: Applications01:17

Radiation: Applications

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The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
The average...
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相关实验视频

Updated: May 12, 2025

Using Generative Art to Convey Past and Future Climate Transitions
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Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

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气候变暖以不可预测的方式改变了资源分配.

Diana S Macias1, Miranda D Redmond1

  • 1Department of Environmental Science, Policy and Management, University of California, Berkeley, CA, USA.

Trends in ecology & evolution
|April 23, 2025
PubMed
概括

气候变暖促进了欧洲种子的生产,但耗尽了树木资源,导致长期生长下降. 这种资源枯竭可能会削弱森林对气候变化影响的整体抵抗力.

科学领域:

  • 生态生态学 生态生态学
  • 林业林业 林业 林业 林业
  • 气候变化科学 气候变化科学

背景情况:

  • 气候变化对物种人口统计的间接影响广泛,但难以量化.
  • 了解资源权衡对于预测森林生态系统反应至关重要.

研究的目的:

  • 调查气候变暖对欧洲 (Fagus sylvatica) 生殖产量的影响以及随后的资源分配.
  • 评估气候驱动的繁殖努力对树木生长和森林恢复力的长期影响.

主要方法:

  • 与气候变量相关的欧洲种子生产的长期数据分析.
  • 评估树木生长和内部资源状况 (例如,碳储备) 在种子生产高的时期之后.

主要成果:

  • 气候变暖与欧洲种子产量增加正相关.
  • 高种子生产导致了内部树木资源的显著耗尽.
  • 资源枯竭导致树木生长的长期下降.

结论:

  • 气候变化引起的种子生产增加可能会给树木带来大量的成本,导致树木的生长减少.
  • 这些发现表明,气候变化可能通过欧洲树的资源枯竭来削弱森林弹性.
关键词:
气候变暖 气候变暖杆是为了杆.生殖生长的权衡.资源预算 资源预算

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  • 在其他树种中也可能存在类似的权衡,这对气候变化下的森林生态系统稳定性有着广泛的影响.