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関連する概念動画

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.
Kepler's Second Law of Planetary Motion01:29

Kepler's Second Law of Planetary Motion

In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. His first law states that all planets orbit the Sun in an elliptical orbit, with the Sun at one of the ellipse's foci. Therefore, the distance of a planet from the Sun varies throughout its revolution around the Sun.
While in an elliptical orbit, the total energy of the planet is conserved. Therefore, the planet slows down when it is at apogee and...
Kepler's First Law of Planetary Motion01:10

Kepler's First Law of Planetary Motion

In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. He formulated his first two laws based on the observations of his forebears, Nikolaus Copernicus and Tycho Brahe.
Polish astronomer Nikolaus Copernicus put forth a theory that stated a heliocentric model for the solar system. According to this heliocentric theory, all the planets, including Earth, orbit the Sun in circular orbits.
On the other hand,...
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.
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...
Kepler's Third Law of Planetary Motion01:18

Kepler's Third Law of Planetary Motion

In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. In 1909, he formulated his first two laws based on the observations of his forebears, Nikolaus Copernicus and Tycho Brahe. However, in 1918, he published his third law of planetary motion, which gives a precise mathematical relationship between a planet's average distance from the Sun and the amount of time it takes to revolve around the Sun. It...

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関連する実験動画

Updated: Jul 12, 2026

Scattering And Absorption of Light in Planetary Regoliths
11:34

Scattering And Absorption of Light in Planetary Regoliths

Published on: July 1, 2019

エアロゾールによる惑星のアルベドの変化.

M A Atwater

    Science (New York, N.Y.)
    |October 2, 1970
    PubMed
    まとめ

    エアロゾールは地球のアルベドに影響を与え,大気の加熱または冷却を引き起こします. エアロゾールの吸収と分散の微妙な変化は,これらの気候の傾向を逆転させることができます.

    科学分野:

    • 大気科学 大気科学
    • 気候科学 気候科学
    • 放射能の移転は,放射能の移転である.

    背景:

    • エアロゾールは,太陽光線と相互作用することで,地球のエネルギーバランスに大きな影響を与える.
    • 惑星のアルベド (温暖化または冷却) に対するエアロゾールの純効果は,それらの光学特性および表面反射性に依存する.
    • これらの相互作用を理解することは,正確な気候モデリングに不可欠です.

    研究 の 目的:

    • エアロゾルの性質が惑星のアルベドとそれに続く大気温の変化にどのように影響するか調査する.
    • エアロゾールの吸収と分散比の変動に対する気候動向の感受性を決定する.
    • 気候ダイナミクスにおけるエアロゾールの光学特性の重要な役割を強調する.

    主な方法:

    • エアロゾールと表面の相互作用を制御する放射線伝送原理の分析.
    • 異なるエアロゾールの光学特性に基づいて惑星のアルベドの変化のモデリング.
    • エアロゾールの吸収と分散比率の時間的変化の検討.

    主要な成果:

    • エアロゾールによる惑星のアルベドの変化の兆候は,エアロゾール吸収/散乱と表面反射性の相互作用によって決定されます.
    • 惑星のアルベドの変化は,大気温暖化または冷却に直接つながります.

    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

    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

    関連する実験動画

    Last Updated: Jul 12, 2026

    Scattering And Absorption of Light in Planetary Regoliths
    11:34

    Scattering And Absorption of Light in Planetary Regoliths

    Published on: July 1, 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

    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

  • エアロゾールの吸収と分散の比率のわずかな変動は,確立された加熱または冷却の傾向の逆転につながる可能性があります.
  • 結論:

    • エアロゾルの放射性効果は,地球の気候システムにおける重要な要因である.
    • エアロゾールの吸収と分散のバランスは,気候強制の重要な決定因子です.
    • エアロゾールの光学特性を監視し,正確に表現することは,将来の気候変動を予測するために不可欠です.