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Thermal Expansion01:22

Thermal Expansion

4.2K
The expansion of alcohol in a thermometer is one of many commonly encountered examples of thermal expansion, which is the change in size or volume of a given system as its temperature changes. The most visible example is the expansion of hot air. When air is heated, it expands and becomes less dense than the surrounding air, which then exerts an upward force on the hot air to, for example, make steam and smoke rise, and hot air balloons float. The same behavior happens in all liquids and gases,...
4.2K
Heating and Cooling Curves02:44

Heating and Cooling Curves

22.2K
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,...
22.2K
Mechanisms of Heat Transfer II01:20

Mechanisms of Heat Transfer II

3.1K
In convection, thermal energy is carried by the large-scale flow of matter. Ocean currents and large-scale atmospheric circulation, which result from the buoyancy of warm air and water, transfer hot air from the tropics toward the poles and cold air from the poles toward the tropics. The Earth’s rotation interacts with those flows, causing the observed eastward flow of air in the temperate zones. Convection dominates heat transfer by air, and the amount of available space for the airflow...
3.1K
Mechanisms of Heat Transfer01:14

Mechanisms of Heat Transfer

152
Heat transfer between the human body and its environment occurs through four main mechanisms: conduction, convection, radiation, and evaporation.
Conduction, accounting for approximately 3% of body heat loss at rest, is the process of exchanging heat between molecules of two materials in direct contact. This can result in both heat loss and gain. For instance, when the body is submerged in water, which conducts heat 20 times more effectively than air, it can either lose or gain significant...
152
The Water Cycle01:00

The Water Cycle

23.9K
The Earth’s hydrosphere includes all of the areas where the storage and movement of water occurs. Since water is the basis of all living processes, the cycling of water is extremely important to ecosystem dynamics.
23.9K
States of Water01:23

States of Water

50.3K
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...
50.3K

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相关实验视频

Updated: May 14, 2025

Thermal Limits Determination for Zooplankton Using a Heat Block
07:16

Thermal Limits Determination for Zooplankton Using a Heat Block

Published on: November 18, 2022

1.3K

湖泊中的地下热浪.

R Iestyn Woolway1, Miraj B Kayastha2,3, Yan Tong4

  • 1School of Ocean Sciences, Bangor University, Menai Bridge, UK.

Nature climate change
|May 12, 2025
PubMed
概括
此摘要是机器生成的。

地下湖泊的热浪频繁,持续时间较长,强度越来越大. 在水面下监测这些极端热水事件对于了解水生生态系统破坏至关重要.

关键词:
水文学的水文学临界技术 临界技术

更多相关视频

Resurrection of Dormant Daphnia magna: Protocol and Applications
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Resurrection of Dormant Daphnia magna: Protocol and Applications

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Subsurface Defect Localization by Structured Heating Using Laser Projected Photothermal Thermography
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Subsurface Defect Localization by Structured Heating Using Laser Projected Photothermal Thermography

Published on: May 15, 2017

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相关实验视频

Last Updated: May 14, 2025

Thermal Limits Determination for Zooplankton Using a Heat Block
07:16

Thermal Limits Determination for Zooplankton Using a Heat Block

Published on: November 18, 2022

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Resurrection of Dormant Daphnia magna: Protocol and Applications
07:37

Resurrection of Dormant Daphnia magna: Protocol and Applications

Published on: January 19, 2018

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Subsurface Defect Localization by Structured Heating Using Laser Projected Photothermal Thermography
11:34

Subsurface Defect Localization by Structured Heating Using Laser Projected Photothermal Thermography

Published on: May 15, 2017

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科学领域:

  • 环境科学 环境科学
  • 水生生态学 水生生态学
  • 气候变化科学 气候变化科学

背景情况:

  • 湖泊热浪,极端热水事件,破坏水生生态系统.
  • 表面热浪已经得到了很好的研究,但它们的垂直结构在很大程度上仍未被探索.

研究的目的:

  • 为了分析地下湖泊热浪的特征.
  • 调查深水和垂直复合热浪的频率,持续时间和强度.

主要方法:

  • 使用了一个时空建模框架.
  • 分析了过去40年的湖泊热浪数据.

主要成果:

  • 地表热浪比地表热浪更频繁,持续时间更长,强度更小.
  • 深水热浪的频率,持续时间和强度显著增加.
  • 近几十年来,垂直复合热浪也在增加.
  • 未来的预测表明热浪模式正在加剧,特别是在高排放的情况下.

结论:

  • 地下热浪是湖泊中一个显著且日益增长的现象.
  • 深水和热浪的频率和强度增加对水生生态系统构成风险.
  • 地下监测对于准确的影响评估和预测湖泊热浪至关重要.