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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.
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...
What is Climate?01:16

What is Climate?

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.
The Carbon Cycle01:14

The Carbon Cycle

Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
What is Weather?01:07

What is Weather?

Overview
Radiation: Applications01:17

Radiation: Applications

The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
The average...

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関連する実験動画

Updated: Jul 11, 2026

Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements
10:22

Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements

Published on: September 7, 2019

人為的なエアロゾールによる気候強制

R J Charlson, S E Schwartz, J M Hales

    Science (New York, N.Y.)
    |January 24, 1992
    PubMed
    まとめ

    トロポスフィアのエアロゾール,特に硫酸エアロゾールは,太陽放射線を反射し,地球を冷却することによって,地球気候に大きな影響を与えます. この冷却効果は,温室効果ガスが引き起こした実質的な地球温暖化を相殺している可能性が高い.

    科学分野:

    • 大気科学 大気科学
    • 気候科学 気候科学
    • 環境科学 環境科学

    背景:

    • トロポスフィアのエアロゾールは以前,地球温暖化における役割として過小評価されていた.
    • 人為的な硫酸エアロゾールは,地球の放射力強引を著しく乱します.

    研究 の 目的:

    • 人為的な硫酸エアロゾールの気候への影響を定量化するために.
    • エアロゾールフォッシングと温室効果ガスのフォッシングを比較する.
    • 気候変動の評価と政策におけるエアロゾールの重要性を強調する.

    主な方法:

    • 人為的な硫酸エアロゾールによる放射線強制の推定.
    • エアロゾールによるフォッシングと温室効果ガスによるフォッシングの比較.
    • フォッシングの地理的および季節的分布の分析.

    主要な成果:

    • 人為的な硫酸エアロゾールは,惑星のアルベドを増やすことで冷却効果を発揮する.
    • 人類による硫酸塩による現在の気候強制は,世界全体で1~2W/m2と推定されています.
    • エアロゾールフォッシングは,温室効果ガスのフォッシングと大きさでは比較できるが,記号的には反対である.

    さらに関連する動画

    Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
    06:27

    Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer

    Published on: May 29, 2019

    Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
    07:32

    Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.

    Published on: June 4, 2021

    関連する実験動画

    Last Updated: Jul 11, 2026

    Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements
    10:22

    Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements

    Published on: September 7, 2019

    Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
    06:27

    Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer

    Published on: May 29, 2019

    Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
    07:32

    Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.

    Published on: June 4, 2021

    結論:

    • エアロゾルの強制放出は,地球温暖化の相当な程度を相殺した可能性がある.
    • フォッシングの地理的,季節的差異は,単純な補償を妨げています.
    • エアロゾールによる気候強制に関する総合的な研究は,気候政策にとって極めて重要です.