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相关概念视频

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.
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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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In convection, thermal energy is carried by the large-scale flow of matter. Ocean currents and large-scale atmospheric circulation, which result from the buoyancy of warm air and water, transfer hot air from the tropics toward the poles and cold air from the poles toward the tropics. The Earth’s rotation interacts with those flows, causing the observed eastward flow of air in the temperate zones. Convection dominates heat transfer by air, and the amount of available space for the airflow...
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Any physical property that depends consistently and reproducibly on temperature can be used as the basis of a thermometer. For example, volume increases with temperature for most substances. This property is the basis for the common alcohol thermometer and the original mercury thermometers. Other properties used to measure temperature include electrical resistance, color, and the emission of infrared radiation.
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Simulating Temperature in a Soil Incubation Experiment
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热冷的地球通过时间

Benjamin J W Mills1

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概括
此摘要是机器生成的。

古代地球

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科学领域:

  • 古气候学
  • 地球系统科学

背景情况:

  • 了解地球过去的气候对于预测未来的气候变化至关重要.
  • 重建古老的气温可以了解长期的气候动态.

研究的目的:

  • 为了重建古代地球的温度记录.
  • 确定和理解全球气候调节系统的机制.

主要方法:

  • 古气候代理的分析 (例如,冰芯,沉积层).
  • 模拟过去的气候条件和系统反.

主要成果:

  • 详细的重建古代的全球温度.
  • 在地质时间尺度上稳定地球温度的自我调节气候系统.

结论:

  • 地球拥有固有的气候调节系统.
  • 这个系统在整个地球历史中起到了维持可居住条件的重要作用.