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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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What is Weather?01:07

What is Weather?

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Overview
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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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Heating and Cooling Curves02:44

Heating and Cooling Curves

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When a substance—isolated from its environment—is subjected to heat changes, corresponding changes in temperature and phase of the substance is observed; this is graphically represented by heating and cooling curves.
For instance, the addition of heat raises the temperature of a solid; the amount of heat absorbed depends on the heat capacity of the solid (q = mcsolidΔT). According to thermochemistry, the relation between the amount of heat absorbed or released by a substance, q, and its...
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Quantifying Heat02:46

Quantifying Heat

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Thermal Energy Microscopically, thermal energy is the kinetic energy associated with the random motion of atoms and molecules. Temperature is a quantitative measure of “hot” or “cold”, which depends on the amount of thermal energy. When the atoms and molecules in an object are moving or vibrating quickly, they have a higher average kinetic energy (KE) (or higher thermal energy), and the object is perceived as “hot”, or it is described as being at a higher temperature. When the...
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Effects of Temperature on Free Energy02:11

Effects of Temperature on Free Energy

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The spontaneity of a process depends upon the temperature of the system. Phase transitions, for example, will proceed spontaneously in one direction or the other depending upon the temperature of the substance in question. Likewise, some chemical reactions can also exhibit temperature-dependent spontaneities. To illustrate this concept, the equation relating free energy change to the enthalpy and entropy changes for the process is considered:
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Thermal Limits Determination for Zooplankton Using a Heat Block
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气候变化带来的湖泊热浪

R Iestyn Woolway1,2, Eleanor Jennings3, Tom Shatwell4

  • 1Centre for Freshwater and Environmental Studies, Dundalk Institute of Technology, Dundalk, Ireland. riwoolway@gmail.com.

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|January 21, 2021
PubMed
概括

由于气候变化, 湖泊热浪, 极端温暖的表面水, 将在全球范围内加剧和延长. 这对湖泊的生物多样性和生态系统服务构成重大风险.

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科学领域:

  • 环境科学
  • 气候科学
  • 石化技术

背景情况:

  • 湖泊生态系统很容易受到温度变化和极端温度的影响.
  • 人们对湖泊热浪及其在全球变暖下的未来知之甚少.

研究的目的:

  • 调查1901年至2099年全球湖泊热浪的变化.
  • 在不同的排放场景下预测未来湖泊热浪的强度和持续时间.

主要方法:

  • 使用卫星观测和数字模型.
  • 分析了全球数百个湖泊.

主要成果:

  • 预计到2100年,湖泊热浪将变得更加热和持续时间更长.
  • 在代表度路径 (RCP) 8. 5下,强度增加到5. 4°C,持续时间为95. 5天.
  • 在RCP 2.6下,强度增加到4. 0°C,持续时间为27. 0天.
  • 较深的湖泊会经历更长时间但不那么强烈的热浪.

结论:

  • 湖泊热浪将加剧气候变暖,影响湖泊的物理和化学特性.
  • 增加热浪的持续时间可能会导致某些湖泊的永久热浪状态.
  • 威胁到水生生物多样性,生态系统的弹性和湖泊提供的重要社会利益.