A User's Manual for DELSOL3 - prod.sandia.gov - Sandia National ...
A User's Manual for DELSOL3 - prod.sandia.gov - Sandia National ...
A User's Manual for DELSOL3 - prod.sandia.gov - Sandia National ...
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A = +0.004013327<br />
B = +0.06476916<br />
C = -0.66956539<br />
D = +0.019276169<br />
E = -0.00051297<br />
Ads is multiplied by the relative atmospheric pressure (PRES or DPRES,<br />
Namelist BASIC) to account <strong>for</strong> the effect of altitude. It is the apparent sun an-<br />
gle, not the actual sun angle, that is tracked by the heliostats.<br />
The default latitude is that <strong>for</strong> Barstow, CA:<br />
X(PLAT) = 35.0'.<br />
II1.B-2. Insolation-The extraterrestrial insolation of the sun, SO, including<br />
the effect of eccentricity of the earth's orbit, is given by (Reference 19):<br />
SO (kw/m2) = 1.353 + 0.045 cos (27r DAY 365.0 + 10.0 1 (1II.B - 7)<br />
where DAY = day of the year.<br />
The position of the sun is symmetric about the summer and winter solstices.<br />
The code ignores the small change in declination during each day and assumes<br />
that sun position is symmetric about noon.<br />
DELSOL assumes clear sky models to predict the direct normal insolation,<br />
S, at the earth's surface. The parameter INSOL controls the insolation model<br />
choice. Insolation is decreased by transmission through the atmosphere. Losses<br />
depend on such factors as the weather, air mass traversed, and altitude, which de-<br />
termine the extent of photon absorption and scattering. The result is that part<br />
of the direct insolation is converted to a diffuse <strong>for</strong>m which cannot be concen-<br />
trated by the heliostats. The annual energy predicted by the clear sky models is<br />
corrected <strong>for</strong> weather effects as described below.<br />
These insolation models are analytical approximations to a widely varying ac-<br />
tual insolation value. That is, measured data <strong>for</strong> a specific location and time may<br />
not agree with the results of any insolation model. For a per<strong>for</strong>mance calculation,<br />
the user should choose a model which, when incorporated with weather consid-<br />
erations, will predict the closest insolation to measured values. For optimization<br />
(design point) calculations and <strong>for</strong> flux map calculations on optimized systems,<br />
the value REFSOL (Namelist BASIC) is used as a fixed insolation value.<br />
a) INSOL = 0, Meinel Model (Reference 20)<br />
S = So{ (1.0 - 0.14ALT)exp(-0.357(sec19~)~~~'*) + O.14ALT) (1II.B - 8)<br />
69