SUMOTOY said:
. In radiant heat it is the passive escape of high temp air without an external pressure device (fan, ram air, ducting, scoop)
Happy to use whatever terms that will help you with differentiating the two types of venting strategies (pun intended). I believe the terms I used are commonplace and accepted in automotive applications, but happy to be more 'technically' correct.
Scott Justusson
It's called forced convection if the fluid motion is caused by a fan, blower, wind ect. It's called free (or natural) covection if the fluid motion is set up by the buoyancy resulting from desity difference cause by the temperature difference with the fluid. Radiant Heat, or Thermal radiation is NOT the passive escape of high temp air.
It's not a matter of being more 'technically' correct. It's either right or wrong. It's either radiant or it's not. What you're talking about is NOT RADIANT HEAT! Doesn't matter if some of your autoshop classmates call it the wrong thing or not. You're wrong - again. Maybe this time you'll have the guts to admit it.
Try wikipedia.org
Thermal radiation is electromagnetic radiation emitted from the surface of an object which is due to the object's temperature. Infrared radiation from a common household radiator or electric heater is an example of thermal radiation, as is the light emitted by a glowing incandescent light bulb. Thermal radiation is generated when heat from the movement of charged particles within atoms is converted to electromagnetic radiation.
The emitted wave frequency of the thermal radiation is a probability distribution depending only on temperature, and for a genuine black body is given by Planck’s law of radiation. Wien's law gives the most likely frequency of the emitted radiation, and the Stefan-Boltzmann law gives the heat intensity.
Convection is the transfer of potential energy, for example heat, by currents within a fluid. Most fluids are liquids, gases, and plasmas, although large solid bodies such as Earth's mantle also behave like a fluid on long time scales and at high pressure and temperature. Thermal convection can arise from temperature differences either within the fluid or between the fluid and its boundary, which maintains a gravitationally unstable density gradient if the temperature gradient increases in the direction of gravity. Other sources of density variations, such as variable composition (for example, salinity), or from the application of an external motive force are also often causes. It is one of the three primary mechanisms of heat transfer, the others being conduction and radiation. Convection occurs in atmospheres, oceans, and planetary mantles.
Free and forced convection
In heat transfer, a distinction is made between free and forced convection.
Free convection is convection in which motion of the fluid arises solely due to the unstable density gradients (for example, the temperature differences existing within the fluid) that can be maintained in the fluid. Example: hot air rising off the surface of a radiator.
The basic premise behind free convection is that heated fluid becomes more buoyant and "rises," while cooler fluid "sinks." Free convection occurs in any liquid or gas which expands or contracts in response to changing temperatures when it is exposed to multiple temperatures in an acceleration field such as gravity or a centrifuge. The local changes in density results in buoyancy forces that cause currents in the fluid. In zero gravity, because buoyancy no longer becomes a factor, free convection does not occur.
Forced convection happens when motion of the fluid is imposed externally (such as by a pump or fan). Example: a fan-powered heater, where a fan blows cool air past a heating element, heating the air. A person blowing on their food to cool it is using forced convection