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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...
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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.
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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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Heat transfer between the human body and its environment occurs through four main mechanisms: conduction, convection, radiation, and evaporation.
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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...
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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...
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Recent advances in coronal heating.

Ineke De Moortel1, Philippa Browning2

  • 1School of Mathematics and Statistics, University of St Andrews, North Haugh, St Andrews KY16 9SS, UK ineke.demoortel@st-andrews.ac.uk.

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This summary is machine-generated.

Scientists are investigating the solar corona's extreme heat, a puzzle known as the coronal heating problem. This review synthesizes recent findings and modeling to identify the Sun's atmospheric heat source.

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Area of Science:

  • Solar Physics
  • Plasma Physics
  • Astrophysics

Background:

  • The solar corona is significantly hotter than the Sun's surface, posing a major scientific challenge.
  • Understanding the coronal heating problem is crucial for explaining energy transfer in the Sun's outer atmosphere.

Purpose of the Study:

  • To review recent observational and modeling advancements related to the solar coronal heating problem.
  • To identify key themes and future research directions for understanding solar atmospheric heating mechanisms.

Main Methods:

  • Synthesis of recent observational findings in solar physics.
  • Overview of large- and small-scale numerical modeling of solar atmospheric processes.
  • Analysis of physical processes relevant to proposed heating mechanisms.

Main Results:

  • Recent research highlights various observational data and simulation results.
  • Multiple physical processes are considered as potential contributors to coronal heating.
  • The review identifies recurring themes across different research approaches.

Conclusions:

  • The coronal heating problem remains an active area of research with ongoing challenges.
  • Future research requires tackling identified challenges in both observation and modeling.
  • A comprehensive understanding necessitates integrating diverse findings on solar atmospheric energy.