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相关概念视频

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...
Graphs of Two-Variable Functions01:27

Graphs of Two-Variable Functions

A weather map provides a practical example of a function of two variables. Across a wide region such as the United States, temperatures vary from one location to another. Each location can be identified by two geographic coordinates: longitude and latitude. Since a single temperature value is assigned to each coordinate pair, the situation can be represented mathematically as a function with two inputs and one output.In mathematical notation, longitude and latitude can be labeled as x and y,...
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 10, 2026

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
13:38

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats

Published on: October 26, 2019

在最后一个冰川时期,南极洲和格陵兰岛的千年级气候变化的时间表.

T Blunier1, E J Brook

  • 1Department of Geosciences, Guyot Hall, Princeton University, Princeton, NJ 08544, USA. blunier@princeton.edu

Science (New York, N.Y.)
|January 6, 2001
PubMed
概括

来自格陵兰岛和南极洲的古气温记录揭示了"双极"模式. 南极的变暖在格陵兰的变暖之前已经有数千年了,这表明海洋远程连接会影响气候变化.

科学领域:

  • 古气候学 古气候学
  • 气候科学 气候科学
  • 冰芯分析 冰芯分析

背景情况:

  • 了解过去的气候动态对于预测未来的气候变化至关重要.
  • 千年规模的气候变化提供了对地球复杂气候系统的见解.

研究的目的:

  • 为了确定格陵兰岛和西南极的古气温到9万年前的精确相对时间表.
  • 为了研究南极和格陵兰岛变暖事件之间的时间关系.
  • 为半球气候远程连接提供证据.

主要方法:

  • 来自格陵兰冰盖项目2和伯德冰芯的大气甲记录的相关性.
  • 开发精确的相对时间表,用于古气温重建.
  • 对两半球千年级温度趋势的分析.

主要成果:

  • 考古温度的相对时间表被延伸到9万年前.
  • 在南极洲发生的七次主要的千年级变暖比格陵兰岛的变暖早了15003000年.
  • 南极的变暖通常发生在温度逐渐上升的过程中,而格陵兰则经历了温度的下降或恒定.

结论:

  • 观察到的模式支持该理论.

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相关实验视频

Last Updated: Jul 10, 2026

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
13:38

Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats

Published on: October 26, 2019

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Simulating Impacts of Ice Storms on Forest Ecosystems

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Using Generative Art to Convey Past and Future Climate Transitions

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  • 双相双极看看看看看看的
  • 对于空气温度变化的假设.
  • 一个海洋远程连接可能将半球之间的气候变化与千年时间尺度联系起来.
  • 这项研究完善了我们对过去冰川时期半球间气候合的理解.