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Solar Energy Perspectives - IEA

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Chapter 2: The solar resource and its possible uses<br />

Figure 2.11 Global normal (top) and direct normal (bottom) Irradiance<br />

180 W<br />

Global normal irradiance (GNI)<br />

90 o<br />

W<br />

90 o<br />

E<br />

180 o<br />

E<br />

60 o<br />

N<br />

60 o<br />

S<br />

30 o<br />

N<br />

30 o<br />

S<br />

0 o<br />

4 000 kWh/m 2 /y<br />

3 750 kWh/m 2 /y<br />

3 500 kWh/m 2 /y<br />

3 250 kWh/m 2 /y<br />

3 000 kWh/m 2 /y<br />

2 750 kWh/m 2 /y<br />

2 500 kWh/m 2 /y<br />

2 250 kWh/m 2 /y<br />

2 000 kWh/m 2 /y<br />

1 750 kWh/m 2 /y<br />

1 500 kWh/m 2 /y<br />

1 250 kWh/m 2 /y<br />

1 000 kWh/m 2 /y<br />

750 kWh/m 2 /y<br />

500 kWh/m 2 /y<br />

Direct normal irradiance (DNI)<br />

60 o<br />

N<br />

60 o<br />

S<br />

30 o<br />

N<br />

30 o<br />

S<br />

0 o<br />

4 000 kWh/m 2 /y<br />

3 750 kWh/m 2 /y<br />

3 500 kWh/m 2 /y<br />

3 250 kWh/m 2 /y<br />

3 000 kWh/m 2 /y<br />

2 750 kWh/m 2 /y<br />

2 500 kWh/m 2 /y<br />

2 250 kWh/m 2 /y<br />

2 000 kWh/m 2 /y<br />

1 750 kWh/m 2 /y<br />

1 500 kWh/m 2 /y<br />

1 250 kWh/m 2 /y<br />

1 000 kWh/m 2 /y<br />

750 kWh/m 2 /y<br />

500 kWh/m 2 /y<br />

180 o<br />

W<br />

o 0 o 90 E<br />

90 o<br />

W<br />

0 o<br />

o<br />

180 o<br />

E<br />

Notes: Global normal irradiance offers the maximum resource and requires two-axis sun-tracking (top). Two-axis sun-tracking with<br />

concentration devices leads to direct normal irradiance (bottom), losing the diffuse component.<br />

Source: Breyer and Schmidt, 2010b.<br />

Key point<br />

Tracking increases the collected energy; concentration narrows it to direct light.<br />

Knowing the resource is key to its exploitation<br />

As the solar resource varies in large proportion with location and time-scales, a solar project<br />

of any kind requires a good amount of knowledge on the actual resource. This requires<br />

assessing not only the overall global solar energy available, but also the relative magnitude<br />

of its three components: direct-beam irradiance, diffuse irradiance from the sky including<br />

clouds, and irradiance by reflection from the ground surface. Also important are the patterns<br />

of seasonal availability, variability of irradiance, and daytime temperature on site. As seen<br />

above, long-term measurement is necessary to avoid being misled by the annual variability,<br />

especially in temperate regions.<br />

43<br />

© OECD/<strong>IEA</strong>, 2011

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