{"id":2621,"date":"2015-10-31T18:25:35","date_gmt":"2015-10-31T23:25:35","guid":{"rendered":"http:\/\/huewhite.com\/umb\/?p=2621"},"modified":"2015-10-31T18:25:35","modified_gmt":"2015-10-31T23:25:35","slug":"another-approach-to-solar-ctd-2","status":"publish","type":"post","link":"https:\/\/huewhite.com\/umb\/2015\/10\/31\/another-approach-to-solar-ctd-2\/","title":{"rendered":"Another Approach to Solar, Ctd"},"content":{"rendered":"<p>A reader asks about those new <a href=\"https:\/\/huewhite.com\/umb\/2015\/10\/30\/another-approach-to-solar-ctd\" target=\"_blank\">solar panels<\/a>:<\/p>\n<blockquote><p><span data-reactid=\".4e.1:5.1:$comment1157750854252545_1159868404040790\/=10.0.$right.0.$left.0.0.2\"><span data-ft=\"{&quot;tn&quot;:&quot;K&quot;}\" data-reactid=\".4e.1:5.1:$comment1157750854252545_1159868404040790\/=10.0.$right.0.$left.0.0.2.$comment-body\"><span class=\"UFICommentBody\" data-reactid=\".4e.1:5.1:$comment1157750854252545_1159868404040790\/=10.0.$right.0.$left.0.0.2.$comment-body.0\"><span data-reactid=\".4e.1:5.1:$comment1157750854252545_1159868404040790\/=10.0.$right.0.$left.0.0.2.$comment-body.0.$end\/=1$text0\/=010\">Is it possible to predict where this will work, i.e. in areas with lots of sunlight. Everywhere in the world? It depends?<\/span><\/span><\/span><\/span><\/p><\/blockquote>\n<p>It depends.<\/p>\n<p>Let&#8217;s start with the ultraviolet side of things.\u00a0 <strong>UV<\/strong> consists of two bands, <strong>UVA<\/strong> (wavelength of 315\u2013400 nm) and <strong>UVB<\/strong> (280\u2013315), courtesy <a href=\"https:\/\/en.wikipedia.org\/wiki\/Ultraviolet#Solar_ultraviolet\" target=\"_blank\"><em><strong>Wikipedia<\/strong><\/em><\/a>.\u00a0 This division is important because UVA is not absorbed by the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Ozone_layer\" target=\"_blank\"><em>ozone layer<\/em><\/a>, while UVB is mildly to mostly absorbed by the ozone layer (there&#8217;s also a UVC layer, which is completely absorbed and also carries some energy).\u00a0 From the <em><strong><a href=\"http:\/\/www.windows2universe.org\/sun\/spectrum\/multispectral_sun_overview.html\" target=\"_blank\">Windows to the Universe<\/a><\/strong><\/em> solar emission chart,<\/p>\n<blockquote><p><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/i1.wp.com\/www.windows2universe.org\/sun\/spectrum\/solar_em_spectrum_smoothed_graph.gif?resize=732%2C428\" alt=\"Solar EM Spectrum - smoothed\" width=\"732\" height=\"428\" \/><\/p><\/blockquote>\n<p>we can see that UVA, which is closer to the visible spectrum than UVB, also carries more energy than does UVB.\u00a0 Since UVA isn&#8217;t absorbed by the ozone layer, the depth of the ozone layer at the location of interest (or the altitude of the site, for that matter) isn&#8217;t as important as it might be.\u00a0 It&#8217;s not irrelevant, since UVB is carrying some of the energy we&#8217;re interested in harvesting, but it&#8217;s not paramount.\u00a0 My quick research suggests the ozone layer becomes thinner at altitude (thus pilots&#8217; concerns about cataracts caused by solar rays and sunburn) as well as at the higher latitudes, i.e., near the poles.\u00a0 So at higher altitudes and latitudes you may receive a little more harvestable energy.<\/p>\n<p>What about infrared?\u00a0 Turns out it, too, has problems reaching the Earth&#8217;s surface.\u00a0 <em><strong>Windows to the World<\/strong><\/em> has another <a href=\"http:\/\/www.windows2universe.org\/earth\/Atmosphere\/earth_atmosph_radiation_budget.html\" target=\"_blank\">handy chart<\/a>:<\/p>\n<blockquote><p><img data-recalc-dims=\"1\" loading=\"lazy\" decoding=\"async\" src=\"https:\/\/i0.wp.com\/www.windows2universe.org\/earth\/Atmosphere\/images\/em_radiation_atmosph_depth_stsci.jpg?resize=475%2C420\" alt=\"Solar EM radiation penetration in Earth's atmosphere\" width=\"475\" height=\"420\" \/><\/p><\/blockquote>\n<p>What is absorbing the radiation?\u00a0 According to the <a href=\"http:\/\/www.ces.fau.edu\/nasa\/module-2\/how-greenhouse-effect-works.php\" target=\"_blank\"><em><strong>Climate Science Investigations<\/strong><\/em><\/a> site, CO<sub>2<\/sub> is highly absorbent:<\/p>\n<blockquote><p><strong>Carbon dioxide (CO2)<\/strong> is also an important greenhouse gas. It has a long lifetime in Earth&#8217;s atmosphere. Carbon dioxide strongly absorbs energy with a wavelength of 15 \u03bcm (micrometers). This makes carbon dioxide a good absorber of wavelengths falling in the infrared radiation region of the spectrum.<\/p><\/blockquote>\n<p>This explains why CO<sub>2<\/sub> is classed as a climate change gas &#8211; by absorption, the gas warms.\u00a0 And there&#8217;s lots of CO<sub>2<\/sub>.\u00a0 More or less evenly distributed, so siting your installation based on infrared considerations doesn&#8217;t appear to be an effective strategy, insofar as this amateur (me!) can tell.<\/p>\n<p>There are other factors as well.\u00a0 The tilt of the Earth relative to its orbital plane (the source of our seasons, basically) means differing levels of solar radiation reaching a given location on Earth varies with the season.\u00a0 The location itself defines the angle of incidence, as moderated by the season.\u00a0 Yet, interestingly enough, a location directly on the equator may not be as effective as a location at 20 degrees latitude, because wet tropical forests will screen out the rays, while at 20 degrees there are a number of dry deserts.<\/p>\n<p>So, yeah, it depends.\u00a0 Having gone through all this, I have to wonder if these are going to be a gimmick, or part of a larger array where the visible spectrum is also harvested.\u00a0 The diagram from Windows to the World certainly\u00a0 clarifies just how much radiation the Earth&#8217;s atmosphere (and magnetic belts) screen out, and what is the best part of the spectrum to harvest &#8211; the visible spectrum.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>A reader asks about those new solar panels: Is it possible to predict where this will work, i.e. in areas with lots of sunlight. Everywhere in the world? It depends? It depends. Let&#8217;s start with the ultraviolet side of things.\u00a0 UV consists of two bands, UVA (wavelength of 315\u2013400 nm) \u2026 <a class=\"continue-reading-link\" href=\"https:\/\/huewhite.com\/umb\/2015\/10\/31\/another-approach-to-solar-ctd-2\/\"> Continue reading <span class=\"meta-nav\">&rarr; <\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"nf_dc_page":"","_jetpack_memberships_contains_paid_content":false,"footnotes":""},"categories":[1],"tags":[],"class_list":["post-2621","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"jetpack_featured_media_url":"","jetpack_sharing_enabled":true,"_links":{"self":[{"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/posts\/2621","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/comments?post=2621"}],"version-history":[{"count":8,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/posts\/2621\/revisions"}],"predecessor-version":[{"id":2629,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/posts\/2621\/revisions\/2629"}],"wp:attachment":[{"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/media?parent=2621"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/categories?post=2621"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/tags?post=2621"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}