|
- Convection (heat transfer) - Wikipedia
Although often discussed as a distinct method of heat transfer, convective heat transfer involves the combined processes of conduction (heat diffusion) and advection (heat transfer by bulk fluid flow) Convection is usually the dominant form of heat transfer in liquids and gases
- Convection | Definition, Examples, Types, Facts | Britannica
convection, process by which heat is transferred by movement of a heated fluid such as air or water Natural convection results from the tendency of most fluids to expand when heated—i e , to become less dense and to rise as a result of the increased buoyancy
- CONVECTIVE Definition Meaning - Merriam-Webster
The meaning of CONVECT is to transfer heat by convection
- Convection: Definition and Examples - Science Facts
Convection is of two types – natural and forced Natural convection is due to buoyancy and the buoyant force acting on the fluid For natural convection to occur, there has to be a temperature difference across the fluid Examples of natural convection include sea breeze and land breeze
- Heat Transfer – Conduction, Convection, Radiation
Convection is heat transfer via the movement of a fluid, such as air or water Heating water on a stove is a good example The water at the top of the pot becomes hot because water near the heat source rises Another example is the movement of air around a campfire Hot air rises, transferring heat upward
- Convection: What Is It How Does It Work? - Sciencing
Convection is a type of heat transfer (similar to conduction or radiation) that operates on the physical movement of particles that creates a physical transfer and cycle of energy
- What is Convection? - BYJUS
Convection is the process of heat transfer by the bulk movement of molecules within fluids such as gases and liquids The initial heat transfer between the object and the fluid takes place through conduction, but the bulk heat transfer happens due to the motion of the fluid
- CONVECTION | English meaning - Cambridge Dictionary
Warm air rises by the process of convection This gradient, established and maintained by the surface buoyancy flux through the process of turbulent convection, is what draws fluid in from the external reservoir
|
|
|