Phonon ( quantized lattice vibration wave ) is a central thermal energy carrier contributing to heat capacity ( sensible heat storage ) and conductive heat transfer in condensed phase, and plays very important role in thermal energy conversion.
32.
Since the majority of the cooling process results from removing sensible heat through radiant exchange with people and objects and not air, occupant thermal comfort can be achieved with warmer interior air temperatures than with air based cooling systems.
33.
As a result, devices were shown to produce this effect reliably, and the term " thermoscope " was adopted because it reflected the changes in sensible heat ( the concept of temperature was yet to arise ).
34.
In the case of pure carbon or carbon monoxide, the two heating values are almost identical, the difference being the sensible heat content of carbon dioxide between 150 �C and 25 �C ( sensible heat exchange causes a change of temperature.
35.
In the case of pure carbon or carbon monoxide, the two heating values are almost identical, the difference being the sensible heat content of carbon dioxide between 150 �C and 25 �C ( sensible heat exchange causes a change of temperature.
36.
Since the membrane is the only barrier blocking the mass transport, relatively high surface related permeate flows can be achieved with DCMD . A disadvantage is the high sensible heat loss, as the insulating properties of the single membrane layer are low.
37.
Air conditioning is concerned with both latent heat ( which involves temperature and relative humidity ), and sensible heat, which is temperature alone . "'( talk ) "'18 : 09, 6 September 2013 ( UTC)
38.
In this context, when the magnitude of B is less than one, a greater proportion of the available energy at the surface is passed to the atmosphere as latent heat than as sensible heat, and the converse is true for values of B greater than one.
39.
First, in infrared remote sensing methodology the radiation emanates from the mm or less, which may not represent the bulk temperature of the upper meter of ocean due primarily to effects of solar surface heating during the daytime, reflected radiation, as well as sensible heat loss and surface evaporation.
40.
Where \ omega _ 1 is the vertical velocity due to the mean baroclinicity in the atmosphere and \ omega _ 2 is the vertical velocity due to the non-adiabatic heating, which includes the latent heat of condensation, sensible heat radiation, etc . ( Singh & Rathor, 1974 ).
