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相关概念视频

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.
Conditions on Early Earth02:06

Conditions on Early Earth

Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Cause and Effect01:53

Cause and Effect

While variables are sometimes correlated because one does cause the other, it could also be that some other factor, a confounding variable, is actually causing the systematic movement in our variables of interest. For instance, as sales in ice cream increase, so does the overall rate of crime. Is it possible that indulging in your favorite flavor of ice cream could send you on a crime spree? Or, after committing crime do you think you might decide to treat yourself to a cone?
Conditions on Early Earth02:06

Conditions on Early Earth

Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
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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相关实验视频

Updated: Jul 8, 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

古气候:米兰科维奇的因果关系问题

D B Karner, R A Muller

    Science (New York, N.Y.)
    |August 31, 2007
    PubMed
    概括

    米兰科维奇理论表明,北半球的阳光照射驱动了冰川周期. 然而,最近的珊瑚研究质疑它在最后一次冰期结束前的作用,促使对数据进行重新评估.

    科学领域:

    • 古气候学 古气候学
    • 地质物理学 地质物理学

    背景情况:

    • 米兰科维奇理论认为,北半球太阳辐射 (日照) 的变化是全球冰川周期的主要驱动因素.
    • 了解冰川终结对于重建地球气候历史至关重要.

    研究的目的:

    • 评估米兰科维奇理论对第二次冰河期结束的适用性.
    • 讨论全球珊瑚研究的最新发现,这些发现可能会挑战现有的气候模型.

    主要方法:

    • 对全球各个地点的珊瑚数据进行的最新研究的综述.
    • 对阳光照射数据的分析及其与冰川时期的相关性.

    主要成果:

    • 最近的珊瑚研究提供了证据,使米兰科维奇理论对前最后一个冰川结束的直接适用性产生了怀疑.
    • 突出了古气候数据和理论预测之间的差异.

    结论:

    • 目前对冰川周期机制的理解,特别是结局,可能需要修订.
    • 对现有的古气候数据进行批判性和公正的重新审查是必要的,以改进气候模型.

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    Published on: October 25, 2024