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相关概念视频

States of Water01:23

States of Water

Water exists in any one of the three classical states: solid (ice), liquid (water), and gas (steam or water vapor). The state of water depends on i) the intermolecular forces that draw molecules together and ii) the kinetic energy that leads to movements that pull them apart.
Water freezes when the intermolecular forces are greater than the kinetic energy. Unlike most other substances, water is less dense in its solid state than in its liquid state. This is because each water molecule can form...
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.
Heating and Cooling Curves02:44

Heating and Cooling Curves

When a substance—isolated from its environment—is subjected to heat changes, corresponding changes in temperature and phase of the substance is observed; this is graphically represented by heating and cooling curves.
For instance, the addition of heat raises the temperature of a solid; the amount of heat absorbed depends on the heat capacity of the solid (q = mcsolidΔT). According to thermochemistry, the relation between the amount of heat absorbed or released by a substance, q, and its...
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: Jun 14, 2026

Simulating Impacts of Ice Storms on Forest Ecosystems
06:27

Simulating Impacts of Ice Storms on Forest Ecosystems

Published on: June 30, 2020

在最后一次冰河时期,淡水迫使气候突然变化.

P U Clark1, S J Marshall, G K Clarke

  • 1Department of Geosciences, Oregon State University, Corvallis, OR 97333, USA. clarkp@ucs.orst.edu

Science (New York, N.Y.)
|July 14, 2001
PubMed
概括

大规模的冰盖波动改变了淡水的路线,影响了北大西洋深水的形成,并在最后一次脱冰过程中引起了气候变化.

科学领域:

  • 古气候学 古气候学
  • 冰川学的冰川学
  • 海洋学 海洋学 海洋学

背景情况:

  • 最后一次降冰的特点是千年规模的冰盖动态.
  • 北美劳伦蒂冰盖的南部边缘经历了相当大的波动.
  • 这些波动发生在大约43°和49°北之间.

研究的目的:

  • 调查劳伦蒂德冰盖边缘波动对北大西洋古海洋学的影响.
  • 了解在最后一次脱冰期间推动气候变化的机制.
  • 探索冰盖驱动的淡水脉冲与海洋循环之间的关系.

主要方法:

  • 分析古气候代理数据以重建冰盖行为和海洋状况.
  • 基于地质证据的冰边缘重建.
  • 海洋学建模以评估淡水流动的影响.

主要成果:

  • 冰盖边缘波动偶尔增加了北大西洋的淡水排放.
  • 大陆的排水被从密西西比河的排水转向哈德逊河或圣劳伦斯河.
  • 增加的淡水流与减少的北大西洋深水形成相吻合.

结论:

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Last Updated: Jun 14, 2026

Simulating Impacts of Ice Storms on Forest Ecosystems
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08:20

In Situ Soil Moisture Sensors in Undisturbed Soils

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  • 冰盖的动态极大地影响了北大西洋的海洋循环和气候.
  • 来自融化冰盖的淡水脉冲提供了气候突然变化的机制.
  • 这种机制很可能是中等全球冰量时期的特征.