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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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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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Temperature Measurement Sites01:14

Temperature Measurement Sites

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A thermometer measures body temperature. The common sites for measuring body temperature are the oral cavity, axillary region, temporal artery, and skin surface, such as the forehead, abdomen, and axilla. True core body temperature is assessed in the rectum, tympanic membrane, pulmonary artery, esophagus, and urinary bladder.
Oral: When assessing oral temperature, the thermometer tip should be placed under the tongue in the posterior sublingual pocket. It offers accurate readings and can be...
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Isothermal Processes01:21

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A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
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Temperature Dependent Deformation01:12

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In a nonhomogeneous rod made up of steel and brass, restrained at both ends and subjected to a temperature change, several steps are involved in calculating the stress and compressive load. Due to the problem's static indeterminacy, one end support is disconnected, allowing the rod to experience the temperature change freely. Next, an unknown force is applied at the free end, triggering deformations in the rod's steel and brass portions. These deformations are then calculated and added...
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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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自最后一个冰河最大期以来的全球表面温度

Matthew B Osman1, Jessica E Tierney2, Jiang Zhu3

  • 1Department of Geosciences, University of Arizona, Tucson, AZ, USA. mattosman@arizona.edu.

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超过24000年的气候变化显示了由冰盖,温室气体,海洋循环和阳光带来的温度变化. 与古气候记录相比, 现代气候变暖的速度和规模是前所未有的.

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科学领域:

  • 古气候学与地球系统科学
  • 气候建模和数据同化

背景情况:

  • 了解过去的气候变化对于预测未来地球系统对外部强迫的反应至关重要.
  • 之前使用气候模型和代理数据的研究已经得出了有关过去气候变化的矛盾结论.

研究的目的:

  • 在过去的2万4千年里,
  • 确定在此期间导致温度变化的主要气候机制.
  • 将最近的变暖趋势与长期的古气候变化进行比较.

主要方法:

  • 用古气候数据同化结合气候模型模拟和代理数据.
  • 对表面温度变化进行了200年分辨率的重新分析.
  • 分析的重点是冰盖和温室气体的辐射强迫,以及海洋循环和阳光照射的变化.

主要成果:

  • 温度变化主要是由辐射强迫和海洋/阳光照射变化驱动的.
  • 全球平均气温自全新世纪初以来稳步上升约0.5°C.
  • 与过去24,000年相比, 现代气候变暖的速度和程度是前所未有的.

结论:

  • 这项研究提供了过去24,000年气候变化的统一观点.
  • 当在长期的古气候背景下观察时,现代变暖的速度和程度都是异常的.
  • 这项研究强调了当前气候趋势与自然变化有很大不同.