{"id":1723,"date":"2017-05-25T03:21:18","date_gmt":"2017-05-25T03:21:18","guid":{"rendered":"http:\/\/blogs.lincoln.ac.nz\/gis\/?p=1723"},"modified":"2023-05-07T03:45:08","modified_gmt":"2023-05-07T03:45:08","slug":"map-projections-part-2-the-allegory-of-the-cave","status":"publish","type":"post","link":"https:\/\/blogs.lincoln.ac.nz\/gis\/map-projections-part-2-the-allegory-of-the-cave\/","title":{"rendered":"Map Projections Part 2: The Allegory of the Cave"},"content":{"rendered":"<p><em>In this second post on map projections we cover the range of different types of projections.\u00a0 Part 1 gave us a broad overview of <a href=\"http:\/\/blogs.lincoln.ac.nz\/gis\/where-on-earth-are-we\/\" target=\"_blank\" rel=\"noopener noreferrer\">different map projections<\/a><\/em><\/p>\n<p>In thinking about map projections I&#8217;m reminded of an <a href=\"http:\/\/webspace.ship.edu\/cgboer\/platoscave.html\" target=\"_blank\" rel=\"noopener noreferrer\">old story<\/a>.\u00a0 Now bear with me on this one: in this story, imagine some prisoners, chained in a cave all their lives, their heads unable to turn such that all they can see in front of them is the cave wall.\u00a0\u00a0 Behind them, a great fire burns, and in between prisoners and fire, puppetters march past with their puppets held high so that they cast shadows on the cave wall.\u00a0 It looks something like this:<\/p>\n<p><a href=\"https:\/\/d-blogs.lincoln.ac.nz\/gis\/wp-content\/uploads\/sites\/3\/2017\/05\/plato_cave.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-full wp-image-1724\" src=\"https:\/\/d-blogs.lincoln.ac.nz\/gis\/wp-content\/uploads\/sites\/3\/2017\/05\/plato_cave.jpg\" alt=\"\" width=\"382\" height=\"274\" srcset=\"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-content\/uploads\/sites\/3\/2017\/05\/plato_cave.jpg 382w, https:\/\/blogs.lincoln.ac.nz\/gis\/wp-content\/uploads\/sites\/3\/2017\/05\/plato_cave-300x215.jpg 300w\" sizes=\"auto, (max-width: 382px) 100vw, 382px\" \/><\/a><\/p>\n<p>The idea here is that the prisoners, not knowing anything else, take the shadows to be reality.\u00a0 The shadows have become how they understand the world.\u00a0 In another part of the story, a prisoner breaks free and emerges from the cave, sees the sun for the first time and realises that things were not at all the way they seemed, and it&#8217;s all a bit frightening.\u00a0 (Sorry, there&#8217;s really not a happy ending to this story.\u00a0 Well, there is&#8230;sort of&#8230;but it&#8217;s not your typical Hollywood blockbuster ending.)<\/p>\n<p><strong>Map Projections<\/strong><\/p>\n<p>Okay, so I&#8217;ll admit, I&#8217;ve got some issues with this story too, but what does it have to do with map projections?\u00a0\u00a0 Like the prisoners, what we see on maps is a bit like the shadows thrown on the cave wall.\u00a0 In fact, the reason they&#8217;re called projections is because map makers originally used shadows cast on a surface to translate the 3D earth onto a flat, 2D plane.\u00a0 Imagine (if you will) a spherical globe constructed with a metal frame of meridians of longitude, parallels of latitude and the land masses.\u00a0 Also imagine a light bulb at the center of this globe.\u00a0 Take a large piece of paper and shape it into a cylinder.\u00a0 Place that cylinder over the globe so it touches at the equator and turn the light on.\u00a0 Now trace the outline of the shadows on the cylinder, et voila!\u00a0 Unroll the paper and you&#8217;ve got a projected map.<\/p>\n<figure id=\"attachment_1725\" aria-describedby=\"caption-attachment-1725\" style=\"width: 366px\" class=\"wp-caption alignnone\"><a href=\"https:\/\/sciencedemonstrations.fas.harvard.edu\/presentations\/mercator-projection\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-1725 size-full\" src=\"https:\/\/d-blogs.lincoln.ac.nz\/gis\/wp-content\/uploads\/sites\/3\/2017\/05\/mercator_projection.jpg\" alt=\"https:\/\/sciencedemonstrations.fas.harvard.edu\/presentations\/mercator-projection\" width=\"366\" height=\"481\" srcset=\"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-content\/uploads\/sites\/3\/2017\/05\/mercator_projection.jpg 366w, https:\/\/blogs.lincoln.ac.nz\/gis\/wp-content\/uploads\/sites\/3\/2017\/05\/mercator_projection-228x300.jpg 228w\" sizes=\"auto, (max-width: 366px) 100vw, 366px\" \/><\/a><figcaption id=\"caption-attachment-1725\" class=\"wp-caption-text\"><em><a href=\"https:\/\/sciencedemonstrations.fas.harvard.edu\/presentations\/mercator-projection\" target=\"_blank\" rel=\"noopener noreferrer\">https:\/\/sciencedemonstrations.fas.harvard.edu\/presentations\/mercator-projection<\/a><\/em><\/figcaption><\/figure>\n<p>And like the prisoners, it&#8217;s the shadows that give us our reality. \u00a0 When the paper is unrolled,\u00a0 the technique outlined above gives us the tried and (I was going to say true, <a href=\"http:\/\/blogs.lincoln.ac.nz\/gis\/where-on-earth-are-we\/\">but&#8230;<\/a>) Mercator Projection.\u00a0 <em>(Do check out this <a href=\"https:\/\/sciencedemonstrations.fas.harvard.edu\/presentations\/mercator-projection\" target=\"_blank\" rel=\"noopener noreferrer\">link\u00a0<\/a> where they actually show how this works.)\u00a0<\/em> In a very analog way, this is how map projections work.\u00a0 The main differences between different projections created this way are the kinds of surface the shadows are projection onto.\u00a0 Above, it&#8217;s a cylinder.\u00a0 But we can also use cones, or planes that touch the globe at a point.\u00a0 This gives us the three main types of projections: azimuthal (planar), conic and cylindrical:<\/p>\n<p><a href=\"https:\/\/d-blogs.lincoln.ac.nz\/gis\/wp-content\/uploads\/sites\/3\/2017\/05\/develsurfaces.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-full wp-image-1728\" src=\"https:\/\/d-blogs.lincoln.ac.nz\/gis\/wp-content\/uploads\/sites\/3\/2017\/05\/develsurfaces.jpg\" alt=\"\" width=\"354\" height=\"432\" srcset=\"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-content\/uploads\/sites\/3\/2017\/05\/develsurfaces.jpg 354w, https:\/\/blogs.lincoln.ac.nz\/gis\/wp-content\/uploads\/sites\/3\/2017\/05\/develsurfaces-246x300.jpg 246w\" sizes=\"auto, (max-width: 354px) 100vw, 354px\" \/><\/a><\/p>\n<p>When unfolded, each lays flat and the traced shadows give us what&#8217;s where.\u00a0 Now we&#8217;re really only just beginning to look at the range of possible map projections (there are thousands built from these three simple approaches) especially when we realise (like our prisoners) that we can also work with mathematical projections that use equations to go from 3D to 2D.\u00a0 Here&#8217; a <a href=\"https:\/\/en.wikipedia.org\/wiki\/List_of_map_projections\" target=\"_blank\" rel=\"noopener noreferrer\">small list of projections<\/a> (69 in total, a mere smattering).\u00a0 As noted <a href=\"http:\/\/blogs.lincoln.ac.nz\/gis\/where-on-earth-are-we\/\">earlier<\/a>, with any projection, it&#8217;s impossible to transfer the features on the surface of a sphere onto a flat plane without creating some sort of distortion.\u00a0 As soon as we turn the light on (metaphorically speaking) we sacrifice something: area, shape, bearing, or distance.<\/p>\n<p>Another way we can classify projections is what aspect of the surface they preserve.\u00a0 Here are the main categories:<\/p>\n<ul>\n<li>Direction Preserving (<i>azimuthal or zenithal<\/i>)<\/li>\n<li>Shape Preserving (<i>conformal<\/i> or <i>orthomorphic<\/i>)<\/li>\n<li>Area Preserving (<i>equal-area<\/i> or <i>equiareal<\/i> or <i>equivalent<\/i> or <i>authalic<\/i>)<\/li>\n<li>Distance Preserving (<i>equidistant<\/i>), or<\/li>\n<li>Shortest Route Preserving (<em>gnomonic<\/em>)<\/li>\n<\/ul>\n<p>Often, the choice of which one to use depends on what the maps will be used for.\u00a0 Mercator first drew his map to be used by mariners, so it was designed to preserve bearing (direction) at the cost of shape and area (hence, an overly large Greenland).\u00a0 Sometimes, a projection can be chosen so that it minimises several distortions at one time, a sort of compromise that has been used on many New Zealand maps (we&#8217;ll look at this more closely later on).<\/p>\n<p><strong>Geodetic Datums<\/strong><\/p>\n<p>When talking about map projections we also need to talk abut geodetic datums.\u00a0 We&#8217;ve covered datums a bit <a href=\"http:\/\/blogs.lincoln.ac.nz\/gis\/and-standing-up-straight\/\">already<\/a>; they are mathematical shapes (spheroids, to be exact) that attempt to represent the shape of the earth.\u00a0 <a href=\"http:\/\/www.linz.govt.nz\/data\/geodetic-system\/datums-projections-and-heights\/geodetic-datums\/world-geodetic-system-1984-wgs84\" target=\"_blank\" rel=\"noopener noreferrer\">WGS84<\/a> is one example but there are many others.\u00a0 Each datum has its own geometric parameters and uses latitude and longitude to locate points on the surface, though the same point, say Cathedral Square, may have two different sets of coordinates between two different spheroids.\u00a0 So in a sense, you <em>could<\/em> be in two (or more) places at one time&#8230;\u00a0 (I&#8217;ll show you how another time.)<\/p>\n<p>So lat\/long is used to locate a point on the spheroid surface &#8211; that&#8217;s referred to as the horizontal datum.\u00a0 We also need a vertical datum to measure heights.\u00a0 There&#8217;s a lot I&#8217;m going to gloss over about heights because they&#8217;re often surprisingly not as simple as we think they are, but for now, the vertical datum is a reference point that allows us to say, &#8220;Here be zero&#8221; against which we can determine if other points are above or below it.\u00a0 The most common one we&#8217;re used to is sea level (<a href=\"http:\/\/blogs.lincoln.ac.nz\/gis\/keeping-our-heads-above-water\/\">and we know how complex <em>that<\/em> can be&#8230;<\/a>).\u00a0 We&#8217;ve already seen how different parts of New Zealand had, until very recently, different vertical datums so it&#8217;s far from simple to get your head around this.<\/p>\n<p>Every map projection is based on a geodetic datum and you can usually find information about that by looking on the map.\u00a0 the geodetic datum is sort of the like the metal globe framework we talked about earlier.\u00a0 The map projection then is how (mathematically) the lat\/long\/height is converted to a flat, Cartesian x, y, z set of coordinates that are shown on the map.\u00a0 I guess in this case, the map projection is like the rays of light in that same example.<\/p>\n<p><strong>My head hurts&#8230;<\/strong><\/p>\n<p>In the next installment of our look at map projections we&#8217;ll focus on projections (and datums) used on New Zealand maps, but before we go, let&#8217;s put some thought into one of the fundamental reasons why we need projections in the first place.\u00a0 Aside from that being how maps are made, there is a more basic reason.<\/p>\n<p>The 3-dimensional nature of latitude and longitude is the best way to specify location on the surface of a spher(oid).\u00a0 Degrees of latitude and longitude can be broken down into divisions of 60 minutes per degree and further into 60 seconds of arc per minute (and there&#8217;s your space-time continuum, maybe).\u00a0 But the big problem with degrees is they not all created equal, particularly when we think about longitude.\u00a0 <em>At the equator<\/em>, a degree of longitude roughly equals 111 km.\u00a0 But as we move north, the meridians converge, such that a degree of longitude reduces to zero at the north and south poles.\u00a0 This makes proper distance measurements a challenge (and why any good navigator worth their salt uses the latitude scales on either side of a chart to make distance measurements rather than the scales across the top and bottom).\u00a0 One nice thing about meters (and we might as well include feet, and leagues, and <a href=\"https:\/\/www.factmonster.com\/math\/measurement\/origins-measurements\" target=\"_blank\" rel=\"noopener noreferrer\">cubits<\/a>) is that a <a href=\"http:\/\/www.surveyhistory.org\/the_standard_meter1.htm\" target=\"_blank\" rel=\"noopener noreferrer\">meter<\/a> is a <a href=\"https:\/\/studiosparis.wordpress.com\/tag\/standard-metre\/\" target=\"_blank\" rel=\"noopener noreferrer\">meter<\/a> is a <a href=\"https:\/\/en.wikipedia.org\/wiki\/Metre\" target=\"_blank\" rel=\"noopener noreferrer\">meter<\/a>, no matter where you are.\u00a0 Projections allow us to use maps to make reliable, standard length and area measurements which are crucial is most GIS analyses, not to mention putting things in the correct place.\u00a0 With map projections I don&#8217;t need to tell someone that I live 0.399 degrees away from Lincoln at 43.53 degrees south latitude.<\/p>\n<p>I think I&#8217;ll crawl back into my cave now, where life is much simpler.<\/p>\n<p>C<\/p>\n","protected":false},"excerpt":{"rendered":"<p>In this second post on map projections we cover the range of different types of projections.\u00a0 Part 1 gave us a broad overview of different map projections In thinking about map projections I&#8217;m reminded of an old story.\u00a0 Now bear with me on this one: in this story, imagine some prisoners, chained in a cave [&hellip;]<\/p>\n","protected":false},"author":3,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-1723","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-json\/wp\/v2\/posts\/1723","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-json\/wp\/v2\/comments?post=1723"}],"version-history":[{"count":1,"href":"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-json\/wp\/v2\/posts\/1723\/revisions"}],"predecessor-version":[{"id":4136,"href":"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-json\/wp\/v2\/posts\/1723\/revisions\/4136"}],"wp:attachment":[{"href":"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-json\/wp\/v2\/media?parent=1723"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-json\/wp\/v2\/categories?post=1723"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.lincoln.ac.nz\/gis\/wp-json\/wp\/v2\/tags?post=1723"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}