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相关概念视频

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.
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...
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...
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.
Radiation Pressure: Problem Solving01:09

Radiation Pressure: Problem Solving

The radiation pressure applied by an electromagnetic wave on a perfectly absorbing surface equals the energy density of the wave. The wave's momentum also gets transferred to the surface when an electromagnetic wave is entirely absorbed by it. The rate at which momentum is transmitted to an absorbing surface perpendicular to the propagation direction equals the force on the surface.
The average value of the rate of momentum transfer divided by the absorbing area represents the average force per...

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相关实验视频

Updated: Jul 12, 2026

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

皮纳图博山喷发导致的辐射气候强迫.

P Minnis, E F Harrison, L L Stowe

    Science (New York, N.Y.)
    |March 5, 1993
    PubMed
    概括

    1991年皮纳图博火山爆发导致了由于火山气溶造成的全球显著降温. 这些气溶增加了地球的白度,反射了更多的阳光,导致可测量的辐射强迫异常.

    科学领域:

    • 地球科学 地球科学 地球科学
    • 大气科学 大气科学
    • 气候科学 气候科学

    背景情况:

    • 火山爆发将气溶注入平流层,影响地球的辐射平衡.
    • 以前对火山辐射强迫的评估依赖于间接测量.
    • 1991年6月皮纳图博火山喷发为直接测量提供了独特的机会.

    研究的目的:

    • 为了确定皮纳图博火山喷发后的火山辐射强迫.
    • 提供第一个明确的,直接测量大规模的火山强迫.
    • 分析直接的冷却效应和辐射平衡的变化.

    主要方法:

    • 利用了NASA太空中的地球辐射预算实验 (ERBE) 的辐射流异常.
    • 分析了气溶对短波和长波辐射强迫的影响.
    • 在晴朗和阴云地区量化地球白度的变化.

    主要成果:

    • 直接测量证实了火山爆发后的显著火山辐射强迫.
    • 火山气溶引发了即时和不断增长的冷却效应,直到1991年9月.
    • 气溶通过反射更多的太阳辐射来增加白度,无论是直接还是间接地在阴云地区.

    结论:

    相关实验视频

    Last Updated: Jul 12, 2026

    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

    • 这项研究提供了第一份关于大规模火山辐射强迫的直接证据.
    • 火山气溶显然通过增加地球的白度导致了全球显著的冷却.
    • ERBE数据提供了对主要火山事件对气候影响的关键见解.