{"id":781,"date":"2019-09-20T11:27:38","date_gmt":"2019-09-20T18:27:38","guid":{"rendered":"https:\/\/c21-wp.phas.ubc.ca\/index.php\/solar-energy-in-a-temperate-climate"},"modified":"2019-10-22T12:55:35","modified_gmt":"2019-10-22T19:55:35","slug":"solar-energy-in-a-temperate-climate","status":"publish","type":"article","link":"https:\/\/c21.phas.ubc.ca\/article\/solar-energy-in-a-temperate-climate\/","title":{"rendered":"Solar Energy in a Temperate Climate"},"content":{"rendered":"
We all have seen solar panels. They are mounted on traffic signs, lighthouses (see title photograph), and in our calculators. They are great green sources of energy. So why isn’t every roof in [Vancouver] covered with them? This would reduce our reliance on fossil fuels.<\/p>\n
Let\u2019s learn something about solar panels and do some simple calculations.<\/p>\n
To create electric potential energy (or colloquially speaking electricity) we have to separate positive and negative charges. In batteries, the work required to separate positive and negative charges is done by an electrochemical reaction. In silicon-based solar cells, the work is done by the incoming solar radiation in a quantum process: a visible photon from the sun has enough energy to separate an electron from a silicon atom leaving behind a site that is positively charged, called\u00a0 a \u201chole\u201d (Remember the duality of light, we can treat light as electromagnetic wave or as a stream of particles called photons). Electrons are attracted to the positive site and holes to the negative site, so once we connect a solar panel to some load (for example a light bulb, a motor or a heater) we have a current that can do work on such external load.<\/p>\n
Let\u2019s calculate how much power we can obtain from a solar panel in Vancouver. The solar constant (the amount of solar radiation per m2<\/sup> at the top of the atmosphere) is about 1400 W\/m2<\/sup>. We have on average 12 hours of sunlight a day, which should give us 1400 W\/m2<\/sup> times 12 hours = 16.8 kWh\/m2<\/sup> per day. But according to Natural Resources Canada[note]Natural Resources Canada: Photovoltaic and Solar Resources, http:\/\/pv.nrcan.gc.ca\/index.php?m=r<\/a>[\/note] we can only expect on average 5.2 kWh\/m2 <\/sup>on a surface perpendicular to the direction from the Sun. This is due to atmospheric absorption and cloud cover.<\/p>\n There is another problem. As the Sun\u2019s position changes during the day (differently in each day of the year) it is expensive to keep the panel perpendicular to the direction from the Sun. To do this requires directional alignment in two axes so the panels cannot be fixed to the roof.<\/p>\n As illustrated Figure 1\u00a0 the power of radiation delivered to a given surface depends on the incident angle. Notice that the power contained in a 1 m2<\/sup> column of radiation impacts 1 m2<\/sup> of surface if it falls vertically but 2 m2<\/sup> of surface if it is at an angle of 30 degrees. So at 30 degrees we are getting only \u00bd of power per m2<\/sup>! The angular dependence of the power delivered is:<\/p>\n $P_{\\theta} = P_{90} \\sin(\\theta) \\tag{1}$<\/p>\n where $ P_{90}$ is the power per unit area of radiation impacting the surface from the direction perpendicular to the surface, $\\theta$ is the angle of the surface from the horizontal and $P_{\\theta}$ is the power per unit area of the same radiation impacting the surface from the direction at the angle $\\theta$ from the horizontal.<\/p>\n