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関連する概念動画

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
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.
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.
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...
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 29, 2026

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

火星での気候の変化

C Sagan, O B Toon, P J Gierasch

    Science (New York, N.Y.)
    |September 14, 1973
    PubMed
    まとめ
    この要約は機械生成です。

    火星 火星 火星 火星

    さらに関連する動画

    Simulating Temperature in a Soil Incubation Experiment
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    Published on: March 31, 2023

    関連する実験動画

    Last Updated: Jun 29, 2026

    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

    Simulating Temperature in a Soil Incubation Experiment
    08:39

    Simulating Temperature in a Soil Incubation Experiment

    Published on: October 28, 2022

    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

    科学分野:

    • 惑星科学は惑星科学である.
    • 気候科学 気候科学
    • 地質学 地質学 地質学

    背景:

    • 火星の赤道の曲がりくねった運河は,過去には液体の水があり,大気圧が高いことを示唆しています.
    • 火星の気候の安定性は,大気のアドベクティブの不安定さに影響されています.

    研究 の 目的:

    • 火星の過去における安定した,穏やかな気候の可能性を調査する.
    • 火星の気候変化を誘発するメカニズムを調査する.

    主な方法:

    • 大気のアドベクティブ不安定性の分析.
    • 傾き,太陽の光度,極地帽のアルベドに基づいた気候ダイナミクスのモデリング.

    主要な成果:

    • 2つの安定した火星の気候が特定されました:一つはほぼ存在し,もう一つは~1バーの圧力です.
    • 火星の傾き,太陽の明るさ,極地板のアルベドの変動は,気候の変化を引き起こす可能性があります.
    • 斜率の変動だけでは,過去の大幅な圧力変動を示唆している.

    結論:

    • 火星は,その歴史を通じて劇的な気候変化を経験してきました.
    • これらの気候の変化は,火星の気象学,地質学,および潜在的な生物学に大きな影響を及ぼします.