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Global Climate Change01:50

Global Climate Change

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.
Isothermal Processes01:21

Isothermal Processes

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.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
Isochoric and Isobaric Processes01:21

Isochoric and Isobaric Processes

A thermodynamic process that occurs at constant volume is called an isochoric process. According to the first law of thermodynamics, heat supplied or removed from the system is partially utilized to perform work and change the internal energy of the system. However, in an isochoric process, the volume remains constant. Hence, the work done by the system is zero. Therefore, the exchange of heat changes the internal energy of the system only. 
Suppose 1000 g of water is heated from 40 degrees...
Phase Transitions: Melting and Freezing02:39

Phase Transitions: Melting and Freezing

Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
Precipitation Gravimetry01:03

Precipitation Gravimetry

Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
Microbes and Climate Change01:27

Microbes and Climate Change

Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...

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関連する実験動画

Updated: May 26, 2026

Using Generative Art to Convey Past and Future Climate Transitions
06:10

Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

最後の氷河期最大期における半球間氷床の同期性.

Michael E Weber1, Peter U Clark, Werner Ricken

  • 1Institute of Geology and Mineralogy, University of Cologne, 50674 Cologne, Germany. michael.weber@uni-koeln.de

Science (New York, N.Y.)
|December 7, 2011
PubMed
まとめ

南極と北半球の氷床の前進と後退のタイミングは同期しており,気候強制に関する以前の仮定に異議を唱えました. 遠隔接続は,これらの大規模な氷河現象を半球間で同期した可能性が高い.

科学分野:

  • 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
  • 氷河学 氷河学とは
  • 四次科学とは四次科学である.

背景:

  • 過去の氷河期における南極と北半球の氷床のダイナミクスの同期はよく理解されていません.
  • 既存のモデルは,地表の気候強制が半球間の非同期的な反応を引き起こすべきだと示唆しています.

研究 の 目的:

  • 東南極氷床のウェデル海部門の正確な年代順を確立するために.
  • 南極の氷床のタイミングを北半球の氷床と比較するために.
  • 半球氷床の振る舞いを同期するメカニズムを調査する.

主な方法:

  • [概要に記載されていない具体的な方法]を用いて,ウェッデル海セクターの新しい年代順を策定する.
  • 新しい南極のデータを,北半球と南極の他の氷床部門からの既存の年代表と統合する.
  • 海平面フォースリングと北大西洋の深水形成を含む,潜在的な遠隔接続の分析.

主要な成果:

  • ウェッデル海の氷床の前進と後退は,北半球のほとんどの氷床と並行して,年代測定の不確実性の中で起こった.

さらに関連する動画

Simulating Impacts of Ice Storms on Forest Ecosystems
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Simulating Impacts of Ice Storms on Forest Ecosystems

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Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
13:38

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats

Published on: October 26, 2019

関連する実験動画

Last Updated: May 26, 2026

Using Generative Art to Convey Past and Future Climate Transitions
06:10

Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

Simulating Impacts of Ice Storms on Forest Ecosystems
06:27

Simulating Impacts of Ice Storms on Forest Ecosystems

Published on: June 30, 2020

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
13:38

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats

Published on: October 26, 2019

  • 表面の気候強制だけでは,観測された同期を説明することはできません.
  • データは,北半球の氷床,海平面,北大西洋の循環を南極の氷床接地線に結びつける遠隔接続をサポートしています.

    • 結論:

    • 半球の氷床は,おそらく一斉に前進し,後退した.
    • 北半球の氷床の動態によって引き起こされる海平面と海洋学的変化は,南極の氷床の同期に決定的な役割を果たしました.
    • この発見は,過去の気候変動の変動を理解し,将来の氷床の反応を予測する上で意味を持つ.