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Global Climate Change01:50

Global Climate Change

25.0K
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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What is Weather?01:07

What is Weather?

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Overview
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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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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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Temperature Dependent Deformation01:12

Temperature Dependent Deformation

221
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...
221

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Updated: Oct 13, 2025

Simulating Temperature in a Soil Incubation Experiment
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Simulating Temperature in a Soil Incubation Experiment

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気候変動による表面温度持続の広範な変化

Jingyuan Li1, David W J Thompson2,3

  • 1Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA.

Nature
|November 18, 2021
PubMed
まとめ
この要約は機械生成です。

気候変動は地表の温度持続性を大きく変化させ,気象現象の持続時間に影響を与えます. これらの変化を理解することは 生態系と社会にとって極めて重要です

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関連する実験動画

Last Updated: Oct 13, 2025

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08:39

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In Situ Soil Moisture Sensors in Undisturbed Soils
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In Situ Soil Moisture Sensors in Undisturbed Soils

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Using Generative Art to Convey Past and Future Climate Transitions
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科学分野:

  • 気候科学
  • 大気科学
  • 環境科学

背景:

  • 世界的な気候変動は,平均気温の上昇や地域的な変動を含む,地表の気温パターンの広範な変化を引き起こしています.
  • 気候現象が生態系や社会に与える影響は 持続時間に大きく左右されていて 温度の持続性は重要な要因となっています

研究 の 目的:

  • 21世紀を通して,気候変動に対応して,表面温度の持続性がどのように変化するかを調査する.
  • これらの温度持続の変化の強度と物理的要因を分析する.

主な方法:

  • 4つの異なる地球システムモデルの 150のシミュレーションからの出力を利用しました.
  • 多様な放射性プロセスと大規模ダイナミクスを持つ簡素化されたモデルから組み込まれたシミュレーション.

主要な成果:

  • 気候変化のシミュレーションでは 表面温度の持続性が 広く変化しています
  • これらの変化は海洋地域において 最も顕著で強烈です
  • 物理的なプロセスの幅広い範囲が 持続性の変化を誘発しているようです

結論:

  • 気候変動による地表温度の変化の持続性は強固である.
  • これらの持続変化の改善された理解,シミュレーション,および制約が不可欠です.