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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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気候変動による湖の熱波

R Iestyn Woolway1,2, Eleanor Jennings3, Tom Shatwell4

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

Nature
|January 21, 2021
PubMed
まとめ
この要約は機械生成です。

湖の熱波は 極端に温暖な地表水で 気候変動により 世界的に激化し 長くなるでしょう これは湖の生物多様性と生態系サービスに重大なリスクをもたらします.

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科学分野:

  • 環境科学
  • 気候科学
  • リムノジー

背景:

  • 湖の生態系は 温度変化や 極端な熱に脆弱です
  • 湖の熱波と 地球温暖化によるその未来については ほとんど知られていません

研究 の 目的:

  • 1901年から2099年までの湖の熱波の変化を調査する.
  • 将来の湖の熱波の強度と持続時間を,異なる排出シナリオで予測する.

主な方法:

  • 衛星観測と数値モデルを利用した.
  • 世界中で何百もの湖を分析しました

主要な成果:

  • 湖の熱波は2100年までに 劇的に高温で長くなる見込みです
  • 代表的な濃度経路 (RCP) 8. 5では,強度は5. 4°C,持続時間は95. 5日になる.
  • RCP 2.6では,強度が4. 0°C,持続時間は27. 0日になる.
  • より深い湖は より長く続くが より強い熱波を経験します

結論:

  • 湖の熱波は温暖化効果を悪化させ 湖の物理的・化学的性質に影響を与えます
  • 熱波の持続時間が長くなり,一部の湖では恒常的な熱波状態になる可能性があります.
  • 水中の生物多様性,生態系の回復力,湖がもたらす社会的な恩恵を脅かしています.