Ecosystem model

Sol-air temperature (T_sol-air) is a variable used to calculate cooling load of a building and determine the total heat gain through exterior surfaces. It is an improvement over:

\frac{q}{A} = h_{o} (T_{o} - T_{s})

Where:

$q$ = rate of heat transfer [W]
$A$ = heat transfer surface area [m²]
$h_{o}$ = heat transfer coefficient for radiation (long wave) and convection [W/m²K]
$T_{o}$ = outdoor surroundings' temperature [°C]
$T_{s}$ = outside surface temperature [°C]

The above equation only takes into account the temperature differences and ignores two important parameters, being 1) solar radiative flux; and 2) infrared exchanges from the sky. The concept of T_sol-air was thus introduced to enable these parameters to be included within an improved calculation. The lower formula results:

$T_{s o l - a i r} = T_{o} + \frac{(a \cdot I - Δ Q_{i r})}{h_{o}}$

Where:

$a$ = solar radiation absortivity (surface solar absorptance or the inverse of the solar reflectance of a material) [-]
$I$ = global solar irradiance (i.e. total solar radiation incident on the surface) [W/m²]
$Δ Q_{i r}$ = extra infrared radiation due to difference between the external air temperature and the apparent sky temperature. This can be written as $Δ Q_{i r} = F_{r} * h_{r} * Δ T_{o - s k y}$ [W/m²]

The product $T_{s o l - a i r}$ just found can now be used to calculate the amount of heat transfer per unit area, as below:

$\frac{q}{A} = h_{o} (T_{s o l - a i r} - T_{s})$

An equivalent, and more useful equation for the net heat loss across the whole construction is:

$\frac{q}{A} = U_{c} (T_{i} - T_{s o l - a i r})$

Where:

$U_{c}$ = construction U-value, according to ISO 6946 [W/m²K].
$T_{i}$ = indoor temperature [°C]
$Δ T_{o - s k y}$ = difference between outside dry-bulb air temperature and sky mean radiant temperature [°C]

By expanding the above equation through substituting $T_{s o l - a i r}$ the following heat loss equation is derived:

$\frac{q}{A} = U_{c} (T_{i} - T_{o}) - \frac{U_{c}}{h_{o}} [a \cdot I - F_{r} \cdot h_{r} \cdot Δ T_{o - s k y}]$

The above equation is used for opaque facades in,^[1] and renders intermediate calculation of $T_{s o l - a i r}$ unnecessary. The main advantage of this latter approach is that it avoids the need for a different outdoor temperature node for each facade. Thus, the solution scheme is kept simple, and the solar and sky radiation terms from all facades can be aggregated and distributed to internal temperature nodes as gains/losses.

Note to Editor: Items $F_{r}$ and $h_{r}$ require further definition to complete this article.

References

↑ ISO 13790, Energy performance of buildings — Calculation of energy use for space heating and cooling

Fundamentals volume of the ASHRAE Handbook, ASHRAE, Inc., Atlanta, GA, USA, 2005
Heating and Cooling of Buildings, 2nd ed., Kreider, Curtiss, Rabl, McGraw-Hill, New York, USA, 2002

Ecosystem model

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