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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.
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 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.
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...
Temperature Dependence on Reaction Rate02:55

Temperature Dependence on Reaction Rate

The Collision Theory
Atoms, molecules, or ions must collide before they can react with each other. Atoms must be close together to form chemical bonds. This premise is the basis for a theory that explains many observations regarding chemical kinetics, including factors affecting reaction rates.
The collision theory is based on the postulates that (i) the reaction rate is proportional to the rate of reactant collisions, (ii) the reacting species collide in an orientation allowing contact between...
Threats to Biodiversity01:50

Threats to Biodiversity

There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...

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関連する実験動画

Updated: Jul 11, 2026

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
07:58

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

急速な気候変動が火山の噴火を引き起こすのか?

M R Rampino, S Self, R W Fairbridge

    Science (New York, N.Y.)
    |November 16, 1979
    PubMed
    まとめ

    大規模な火山噴火は,気候変動によって引き起こされる可能性があります. 気候の変動は地殻を変化させ,長期にわたって火山と地震の活動を増加させる可能性があります.

    科学分野:

    • 地球科学 地球科学 地球科学
    • 気候科学 気候科学
    • 火山学 火山学とは

    背景:

    • 大規模な火山噴火は,しばしば10年またはそれ以上の冷却の傾向に続く.
    • 火山の塵のベールが短期的な地球冷却を引き起こしますが,氷河期やより長い気候変化を起こす可能性は低いです.
    • 気候の変動は地殻のストレス変化を引き起こす可能性があります.

    研究 の 目的:

    • 気候変動と火山活動との関係を調査する.
    • 気候の変動が地殻に影響を与え,火山の潜在力を高める可能性のあるメカニズムを探求する.

    主な方法:

    • 歴史的な気候データと火山噴火記録の分析.
    • 気候によって引き起こされる氷と水の質量の変動による地殻のストレス変化のモデリング.
    • 地質学的な出来事に関連して地球の軸とスピンレートの変化の検討.

    主要な成果:

    • 気候によって引き起こされる地殻のストレス変化,例えば氷/水の積載/卸載は,火山および地震の可能性に影響を与える可能性があります.
    • 長期にわたる気候の冷却傾向は,大規模な火山噴火に先立ちます.
    • 塵の覆いは,長期的な気候の安定に限られた影響を及ぼします.

    さらに関連する動画

    Rapid PCR Thermocycling using Microscale Thermal Convection
    09:02

    Rapid PCR Thermocycling using Microscale Thermal Convection

    Published on: March 5, 2011

    Atom Probe Tomography Analysis of Exsolved Mineral Phases
    08:14

    Atom Probe Tomography Analysis of Exsolved Mineral Phases

    Published on: October 25, 2019

    関連する実験動画

    Last Updated: Jul 11, 2026

    Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
    07:58

    Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

    Published on: August 7, 2017

    Rapid PCR Thermocycling using Microscale Thermal Convection
    09:02

    Rapid PCR Thermocycling using Microscale Thermal Convection

    Published on: March 5, 2011

    Atom Probe Tomography Analysis of Exsolved Mineral Phases
    08:14

    Atom Probe Tomography Analysis of Exsolved Mineral Phases

    Published on: October 25, 2019

    結論:

    • 大規模な火山噴火を起こすには,火山塵ではなく,気候の変動が重要な役割を果たす可能性があります.
    • 地球の気候システムと地質学的活動は相互に関連しています.
    • 気候と火山活動との間のフィードバックメカニズムを完全に理解するには,さらなる研究が必要です.