Sensible heat, in contrast to latent heat, is the heat transferred to a thermodynamic system that has as its sole effect a change of temperature.
22.
The atmospheric and oceanic circulation redistributes some of this energy as sensible heat and latent heat partly via the mean flow and partly via eddies, known as cyclones in the atmosphere.
23.
This is a simplistic statement, and there is further reading on sensible heat ratios and the specific heat capacity of air, both of which have an effect on thermal performance ..
24.
Changes of Latent heat is associated with the change of phase of atmospheric water, vaporization and condensation, whereas sensible heat is energy that reflects the temperature of the atmosphere or ocean, or ice.
25.
The atmosphere near the surface is largely opaque to thermal radiation ( with important exceptions for " window " bands ), and most heat loss from the surface is by sensible heat and latent heat transport.
26.
Where ?E is the energy needed to change the phase of water from liquid to gas, R n is the net radiation, G is the soil heat flux and H is the sensible heat flux.
27.
The second source is the internal sensible heat generated from frictional dissipation ( equal to W _ { out } ), which occurs near the surface within the tropical cyclone and is recycled to the system.
28.
Latent heat is associated with changes of state, measured at constant temperature, especially the phase changes of atmospheric water vapor, mostly vaporization and condensation, whereas sensible heat directly affects the temperature of the atmosphere.
29.
The energy introduced into the system while the temperature did not change is called a " latent energy ", or latent heat, in contrast to sensible heat, which is associated with temperature change.
30.
The "'Energy Optimization Furnace "'is a BOF variant associated with a scrap preheater where the sensible heat in the off-gas is used for preheating scrap, located above the furnace roof.
