Jove
Visualize
联系我们

相关概念视频

Mechanism of heat transfer01:19

Mechanism of heat transfer

Understanding heat transfer mechanisms is essential for understanding how our bodies maintain balance in different environmental conditions. When the environment is thermoneutral, the body is in a state of balance, neither using nor releasing energy to maintain its core temperature. However, when the environment is not thermoneutral, the body employs four heat transfer mechanisms to maintain homeostasis: conduction, convection, evaporation, and radiation. These mechanisms facilitate heat...
Absorption of Radiation01:05

Absorption of Radiation

The rate of heat transfer by emitted radiation is described by the Stefan-Boltzmann law of radiation:
Heat Flow and Specific Heat01:12

Heat Flow and Specific Heat

Heat is a type of energy transfer that is caused by a temperature difference, and it can change the temperature of an object. Since heat is a form of energy, its SI unit is the joule (J). Another common unit of energy often used for heat is the calorie (cal), which is defined as the energy needed to change the temperature of 1 g of water by 1 °C, specifically between 14.5 °C and 15.5 °C, since the energy needed shows a slight temperature dependence. Another commonly used unit is the kilocalorie...
Mechanisms of Heat Transfer II01:20

Mechanisms of Heat Transfer II

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...
Quantifying Heat02:46

Quantifying Heat

Thermal Energy Microscopically, thermal energy is the kinetic energy associated with the random motion of atoms and molecules. Temperature is a quantitative measure of “hot” or “cold”, which depends on the amount of thermal energy. When the atoms and molecules in an object are moving or vibrating quickly, they have a higher average kinetic energy (KE) (or higher thermal energy), and the object is perceived as “hot”, or it is described as being at a higher temperature. When the atoms and...
Mechanisms of Heat Transfer I01:14

Mechanisms of Heat Transfer I

Just as interesting as the effects of heat transfer on a system are the methods by which the heat transfer occur. Whenever there is a temperature difference, heat transfer occurs. It may occur rapidly, such as through a cooking pan, or slowly, such as through the walls of a picnic ice box. So many processes involve heat transfer that it is hard to imagine a situation where no heat transfer occurs. Yet, every heat transfer takes place by only three methods: conduction, convection, and radiation.

您也可能阅读

相关文章

通过共同作者、期刊和引用图与本文相关的文章。

排序
Same author

Factors governing tropospheric mean temperature.

Science (New York, N.Y.)·1976
Same author

Aerosol and climate: some further considerations.

Science (New York, N.Y.)·1974
查看所有相关文章
JoVE
x logofacebook logolinkedin logoyoutube logo
关于 JoVE
概览领导团队博客JoVE 帮助中心
作者
出版流程编辑委员会范围与政策同行评审常见问题投稿
图书馆员
用户评价订阅访问资源图书馆顾问委员会常见问题
研究
JoVE JournalMethods CollectionsJoVE Encyclopedia of Experiments存档
教育
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab Manual教师资源中心教师网站
使用条款与条件
隐私政策
政策

相关实验视频

Updated: Jul 12, 2026

Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data
09:55

Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data

Published on: December 12, 2013

净表面加热和厄尔尼诺之间可能存在的联系.

B C Weare

    Science (New York, N.Y.)
    |September 2, 1983
    PubMed
    概括

    局部地表升温对东太平洋地区的厄尔尼诺现象产生重大影响. 大气强迫和海洋动力学在整个厄尔尼诺生命周期中发挥着关键作用.

    科学领域:

    • 海洋学 海洋学 海洋学
    • 大气科学 大气科学
    • 气候动力学 气候动力学

    背景情况:

    • 厄尔尼诺现象是东部热带太平洋的主要空海现象.
    • 了解厄尔尼诺的生命周期对于气候预测至关重要.
    • 局部地表加热在厄尔尼诺现象动态中的作用需要进一步研究.

    研究的目的:

    • 调查局部净表面加热对厄尔尼诺现象的影响.
    • 分析海面温度和热量流动之间的关系.
    • 确定厄尔尼诺现象的前体和促成因素.

    主要方法:

    • 分析了1957年至1976年的每月海洋天气总结.
    • 计算相关性和连贯性谱的计算.
    • 为海洋动态对厄尔尼诺现象的影响开发一个代理变量.

    主要成果:

    • 在赤道太平洋东部的净表面热量流和海面温度之间发现了强烈的相关性.
    • 在南极25度附近发现了一种海温前体,在南极5度附近发生变化之前.
    • 在厄尔尼诺的早期阶段,局部表面加热至关重要; 动态在以后占主导地位.

    结论:

    更多相关视频

    Experimental Methodology for Estimation of Local Heat Fluxes and Burning Rates in Steady Laminar Boundary Layer Diffusion Flames
    10:29

    Experimental Methodology for Estimation of Local Heat Fluxes and Burning Rates in Steady Laminar Boundary Layer Diffusion Flames

    Published on: June 1, 2016

    相关实验视频

    Last Updated: Jul 12, 2026

    Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data
    09:55

    Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data

    Published on: December 12, 2013

    Experimental Methodology for Estimation of Local Heat Fluxes and Burning Rates in Steady Laminar Boundary Layer Diffusion Flames
    10:29

    Experimental Methodology for Estimation of Local Heat Fluxes and Burning Rates in Steady Laminar Boundary Layer Diffusion Flames

    Published on: June 1, 2016

    • 当地净表面加热是厄尔尼诺生命周期的关键驱动因素.
    • 通过表面热量流来强迫大气被认为是一个重要的因素.
    • 热和动态过程都是厄尔尼诺发展和进展的组成部分.