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The Stereographic projection is one of these.Now the straight line is the great circle, and the curved one is the loxodrome. Pin one end to New York and one to Istanbul, and pull the string taut. The one on the left has been set so that the center of the area with the least distortion is around the Great Lakes, while on the right, the map has been centered on southeast Australia. As we discussed above, each projection has places where distortion is worse, and places where it is not too bad. In reality, South America is eight times larger than Greenland. Take a look at these two maps, made with the Azimuthal Equidistant projection:Both use the same projection, but each one has different parameters. If your projection requires a center longitude and/or a center latitude, enter coordinates that are in the center of the area youâre mapping. In the same way, a rectangle and a square have the same general âformâ despite being different shapes, whereas a square and a circle do not.Like equal-area, this property is all-or-nothing; your projection either preserves forms everywhere on the map, or it doesnât preserve them anywhere.A trip from Madison to Buenos Aires is much farther than a trip from Madison to Madrid. This is what makes compromise projections good for world maps. The good news is that map projections allow us to distort systematically; we know exactly how things are being stretched or squashed at any given point. Each has advantages and disadvantages and is better suited to certain situations. We have many different map projections because each has different patterns of distortionâthere is more than one way to flatten an orange peel. As you may imagine, the fact that there are so many means there is no âbestâ projection. The plus side of this is that no place gets ridiculously distorted. They make air and ship navigation easy, because you just have to draw a straight line, point your ship in that direction, and start sailing. Theyâre both still Azimuthal Equidistant projections, meaning they show distances correctly when measured out from the center of the projection, but they each have different center points. This projection does not preserve the âlookâ or the âformâ of places. As in the above example, youâll be setting it so that the projection minimizes distortions in the area youâre mapping.Some projections, such as Albers Equal Area Conic, require that you input By doing this, youâre making sure that no point in your map is very far from a standard lineâfrom one of those places where thereâs no distortion. Likewise with the Earthâif we want to make a map, we need to distort the Earthâs surface to flatten it. Fortunately, we get to pick the place where distortions are minimal when weâre setting up a projection. It stretches or twists or squashes them, instead.
The Stereographic projection is one of these.Now the straight line is the great circle, and the curved one is the loxodrome. Pin one end to New York and one to Istanbul, and pull the string taut. The one on the left has been set so that the center of the area with the least distortion is around the Great Lakes, while on the right, the map has been centered on southeast Australia. As we discussed above, each projection has places where distortion is worse, and places where it is not too bad. In reality, South America is eight times larger than Greenland. Take a look at these two maps, made with the Azimuthal Equidistant projection:Both use the same projection, but each one has different parameters. If your projection requires a center longitude and/or a center latitude, enter coordinates that are in the center of the area youâre mapping. In the same way, a rectangle and a square have the same general âformâ despite being different shapes, whereas a square and a circle do not.Like equal-area, this property is all-or-nothing; your projection either preserves forms everywhere on the map, or it doesnât preserve them anywhere.A trip from Madison to Buenos Aires is much farther than a trip from Madison to Madrid. This is what makes compromise projections good for world maps. The good news is that map projections allow us to distort systematically; we know exactly how things are being stretched or squashed at any given point. Each has advantages and disadvantages and is better suited to certain situations. We have many different map projections because each has different patterns of distortionâthere is more than one way to flatten an orange peel. As you may imagine, the fact that there are so many means there is no âbestâ projection. The plus side of this is that no place gets ridiculously distorted. They make air and ship navigation easy, because you just have to draw a straight line, point your ship in that direction, and start sailing. Theyâre both still Azimuthal Equidistant projections, meaning they show distances correctly when measured out from the center of the projection, but they each have different center points. This projection does not preserve the âlookâ or the âformâ of places. As in the above example, youâll be setting it so that the projection minimizes distortions in the area youâre mapping.Some projections, such as Albers Equal Area Conic, require that you input By doing this, youâre making sure that no point in your map is very far from a standard lineâfrom one of those places where thereâs no distortion. Likewise with the Earthâif we want to make a map, we need to distort the Earthâs surface to flatten it. Fortunately, we get to pick the place where distortions are minimal when weâre setting up a projection. It stretches or twists or squashes them, instead.