Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
07-Bld-A5 Building Science — National Exam, December 2017. Six questions of 20 marks each were printed; per the paper's own NOTES only the first five in the answer book are graded, but all six are answered below as a complete study resource.
Reference texts: ASHRAE Handbook — Fundamentals (Chapters 1 Psychrometrics, 14 Climatic Design Information, 25 Thermal and Water Vapor Transmission Data, 26 Heat, Air, and Moisture Control in Building Assemblies); McQuiston, Parker & Spitler, Heating, Ventilating, and Air Conditioning: Analysis and Design; National Building Code of Canada (NBCC).
Check: two inputs are assumed since they were not in the printed data — (1) clock time is taken as solar time (no equation-of-time/longitude correction, the standard simplification at this exam level); (2) ground reflectance ρᵣ = 0.2, the ASHRAE default for ordinary (non-snow) ground.
Find. Total solar irradiation (direct + diffuse + ground-reflected) on the tilted, east-facing collector at the stated time, using the ASHRAE clear-sky model.
By 2 PM the sun has swung well southwest of the meridian; the east-facing collector is now looking almost edge-on at it, so the direct beam is nearly grazing.
Approach. Find the solar position (declination, hour angle, altitude, azimuth) for the stated place/date/time, resolve the angle of incidence on the tilted east-facing surface, then evaluate the ASHRAE clear-sky direct, diffuse and ground-reflected components and sum them.
Solar declination for day n = 202 (July 21):
$$\delta = 23.45\sin\left(\frac{360(284+n)}{365}\right) = 23.45\sin(479.3^\circ) = 20.44^\circ$$
Hour angle at 2:00 PM, two hours past solar noon (15°/hour): H = 30°.
Solar altitude β, from sinβ = cosL·cosδ·cosH + sinL·sinδ:
$$\sin\beta = \cos(44^\circ)\cos(20.44^\circ)\cos(30^\circ) + \sin(44^\circ)\sin(20.44^\circ) = 0.8262 \Rightarrow \boxed{\beta = 55.7^\circ}$$
Solar azimuth φ (from south, +west), from sinφ = cosδ·sinH/cosβ:
$$\sin\phi = \frac{\cos(20.44^\circ)\sin(30^\circ)}{\cos(55.7^\circ)} = 0.832 \Rightarrow \phi = 56.3^\circ\ \text{(west of south, as expected mid-afternoon)}$$
Angle of incidence θ on the tilted east-facing surface (surface azimuth γ = −90° from south), using
$$\cos\theta = \cos\beta\cos(\phi-\gamma)\sin\Sigma + \sin\beta\cos\Sigma$$
$$\cos\theta = \cos(55.7^\circ)\cos(146.3^\circ)\sin(60^\circ) + \sin(55.7^\circ)\cos(60^\circ) = 0.0074 \Rightarrow \boxed{\theta = 89.6^\circ}$$
An angle of incidence approaching 90° is exactly what is expected: by 2 PM the east-facing collector is nearly edge-on to the sun, which now sits well into the southwest sky.
Direct-normal irradiation, ASHRAE clear-sky model, July constants A = 1085 W/m², B = 0.207:
$$I_{DN} = \frac{A}{\exp(B/\sin\beta)} = \frac{1085}{\exp(0.207/0.826)} = 845\ \text{W/m}^2$$
Direct component on the tilted surface:
$$I_{DT} = I_{DN}\cos\theta = 845\times 0.0074 = 6\ \text{W/m}^2$$
Nearly zero, because the collector is almost edge-on to the beam.