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So in order to get stuff to line up on a map different pieces of data on top of each other we have to use a coordinate system, but the issue is that the actual earth is a really lumpy object it's got topography and bathymetric and even the ocean height you know sea level which to us seems like oh well that's that's the shape of the earth is the ocean well even that changes based on you know whether it's tides or different weather systems or things like that there's different pressure, so there's a whole field of study luckily called geodesy and that's there's an earth scientist that go out and try to measure the earth what they find is that the acceleration of gravity is actually different at different places on the earth which means that the mass of the earth is not spherical it's not even close it's its what they call a gelid it's a geophysical approximation of the earth and I think the kind of easier way to understand is that if the entire surface of the earth were kind of a liquid and there were no wind or tides but only the gravitational field and the rotation of the earth were taken into account what is the shape that that earth would take but lucky for us, we don't actually have to deal with that because as cartographers in GIS practitioners we still need a grid system, so the gelid isn't good enough because it's lumpy we need a clean mathematical object like an ellipsoid to assign values of latitude and longitude so that we can actually locate things on the earth so the lab tune hopefully as you know is it climbs like a ladder like this it measures how high we are off of kind of zero at the equator 90 at the poles, and we'd say plus 90 and negative 90 negative 90 being the South Pole plus 90 being North Pole and latitude and longitude are kind of great because we're like okay well if we have the system we can always know on this ellipsoid it's really an oblate ellipsoid it's kind of just the squat egg-shaped thing where we are anywhere on it using the system, so the problem with the ellipsoid is it doesn't really we can't measure with it so if you can see right here if we were to keep going north in north and north, and we were we actually measure using latitude its consistent latitude one minute of latitude is a nautical mile at the North Pole all the way to the equator to the South Pole but longitude the one that measures kind of east-west direction it starts at the equator as one nautical mile for every minute but as you go north and south away from the equator it kind of gets skinnier and skinnier and skinnier and then suddenly it's at the North Pole exactly it's zero there is no measurement for longitude at the North Pole, so the problem is when our units kind of very so the degrees of longitude are not constant we can't measure we can't reliably measure I should say any kind of area or distance or anything like that so what do we've just figured out okay we know how to locate things on the globe, but we can't measure anything so...
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