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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.
Gas Solubility01:31

Gas Solubility

Gas solubility in liquids forms liquid-gas solutions, such as soft drinks, where carbon dioxide is dissolved in water, and the ocean, where the solubility of oxygen and carbon dioxide supports marine life. The ability of oceans to dissolve gases impacts weather conditions in the troposphere.However, gas-liquid interactions vary. For instance, hydrogen chloride gas is highly soluble in water, while oxygen's solubility is much lower. Because these solutions are non-ideal, Raoult’s law, which...
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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Updated: Jun 24, 2026

Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential
14:38

Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential

Published on: April 20, 2012

1958年の南極におけるオゾンの総量

P A Newman

    Science (New York, N.Y.)
    |April 22, 1994
    PubMed
    まとめ

    塩素ラジカルによって引き起こされる南極のオゾンホールは,1958年には存在しなかった. 1958年のDumont d'Urville駅からのデータは,他のオゾン測定と科学的な理解と矛盾しています.

    科学分野:

    • 大気化学 大気化学
    • オゾン層の研究について
    • 南極科学 南極科学

    背景:

    • 南極のオゾンホールは,塩素ラジカルによる触媒的なオゾン破壊によって引き起こされる年間現象です.
    • 8月に形成され,10月にピークに達し,12月に消えます.

    研究 の 目的:

    • デュモン・ド・ウルヴィルの1958年のオゾン測定の信頼性を評価する.
    • 1958年に南極にオゾンホールは存在していたかどうかを判断するために.

    主な方法:

    • 1958年,ドゥモント・ド・ウルヴィル駅からのスペクトログラフィックプレートの分析.
    • ダンモント板のデータと1958年のドブソン光スペクトロフォトメーターの測定値の比較.
    • 現代の南極観測と気象/理論モデルのデータとの比較によるデータ評価.

    主要な成果:

    • 1958年のDumont d'Urvilleのスペクトログラフィックプレートデータでは,オゾン全体の値が極めて低いことが示されています.
    • この1958年のドゥモント板のデータは,1958年のドブソン光スペクトロフォトメーターの測定値と矛盾しています.
    • 1958年のデュモントのデータは,現在の南極観測と確立された大気モデルと矛盾しています.

    さらに関連する動画

    Measurement of Greenhouse Gas Flux from Agricultural Soils Using Static Chambers
    11:50

    Measurement of Greenhouse Gas Flux from Agricultural Soils Using Static Chambers

    Published on: August 4, 2014

    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: Jun 24, 2026

    Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential
    14:38

    Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential

    Published on: April 20, 2012

    Measurement of Greenhouse Gas Flux from Agricultural Soils Using Static Chambers
    11:50

    Measurement of Greenhouse Gas Flux from Agricultural Soils Using Static Chambers

    Published on: August 4, 2014

    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

    結論:

    • 1958年に南極でオゾンホールの存在を裏付ける信頼できる証拠はありません.
    • 1958年のDumont d'Urvilleのスペクトログラフィのデータは,オゾンホールの存在を評価するために信頼できない.