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Specialty Expressions: EQUIVALENT TEMPERATURE

ExpressionsDomainDefinition
British equivalent temperatureMiningSee: equivalent temperature. (references)
Equivalent temperatureAerospace1. Isobaric equivalent temperature; the temperature that an air parcel would have if all water vapor were condensed out at constant pressure, the latent heat released being used to heat the air, Ti, e = T [1 + (Lw / cp T)] where Ti, e is the isobaric equivalent temperature; T is the temperature; w is the mixing ratio; L is the latent heat; and cp is the specific heat of air at constant pressure. 2. Adiabatic equivalent temperature; The temperature that an air parcel would have after undergoing the following (physically unrealizable) process: dry-adiabatic expansion until saturated; pseudoadiabatic expansion until all moisture is precipitated out; dry-adiabatic compression to the initial pressure. This is the equivalent temperature as read from a thermodynamic chart and is always greater than the isobaric equivalent temperature: Ta, e = T exp (Lw / cp T) where Ta, e is the adiabatic equivalent temperature. Also called pseudoequivalent temperature. (references)
Equivalent temperatureMiningA composite of mean radiant temperature and air temperature; also defined as the mean temperature of the environment effective in controlling the rate of sensible heat loss from a black body in still air when the surface temperature and size of the black body are comparable to those of the human body. Where the enclosure surface (mean radiant temperature) and air temperatures are equal, this temperature is also the British equivalent temperature; when not equal, the British equivalent temperature is that temperature at which a body with an 80 degrees F (26.7 degrees C) surface temperature will lose sensible heat at the same rate as in the given environment. Syn: British equivalent temperature. (references)
Isobaric equivalent temperatureAerospaceSee equivalent temperature, sense 1. (references)
Isobaric equivalent temperaturePhysicsTemperature that an air parcel would have if all water vapor were condensed out at constant pressure, the latent heat released being used to heat the air. Source: European Union. (references)

Source: compiled by the editor from various references; see credits.

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Extended Definition: Equivalent temperature


Equivalent temperature

Equivalent temperature is the temperature of an air parcel from which we would have completely extracted its water vapor content by an adiabatic process.

Air contains water vapor that has been evaporated into it from liquid sources (lakes, sea, etc...). The energy needed to do that has been taken from the air. Taking a volume of air at temperature T and mixing ratio of r , drying it by condensation will restitute energy to the airmass. This will depend on the latent heat release as:

T_e \approx T + \frac {L_v}{c_{pd}} r

\,L_v : latent heat of evaporation (2400 kJ/kg {at 25C} to 2600 kJ/kg {at -40C})

\,c_{pd} : specific heat at constant pressure for air (\approx 1004 J/(kg·K))

Tables exist for exact values of the last two coefficients.

Bibliographie

  • M K Yau and R.R. Rogers, Short Course in Cloud Physics, Third Edition, published by Butterworth-Heinemann, January 1, 1989, 304 pages. EAN 9780750632157 ISBN 0-7506-3215-1
  • J.V. Iribarne and W.L. Godson, Atmospheric Thermodynamics, published by D. Reidel Publishing Company, Dordrecht, Holland, 1973, 222 pages

Source: adapted by the editor from Wikipedia, the free encyclopedia; from the article "Equivalent temperature". Image Credit.