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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 Radiation
The rate of heat transfer by emitted radiation is described by the Stefan-Boltzmann law of radiation:
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 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 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 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.
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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:
- 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.

