![[Image:(x,y)]](Sfigs/Sxy.gif)
The distance on one axis is named "x" and on the other axis "y". Given then a point P, one draws from it lines parallel to the axes, and the values of x and y at their intersections completely define the point. In honor of Descartes, this way of labeling points is known as a cartesian system and the two numbers (x,y) that define the position of any point are its cartesian coordinates.
Graphs use this system, as do some maps.
![[IMAGE:3-D Coord]](Sfigs/S3D.gif)
This works well on a flat sheet of paper, but the real world is 3-dimensional and sometimes it is necessary to label points in 3-dimensional space. The cartesian (x,y) labeling can be extended to 3 dimensions by adding a third coordinate z. If (x,y) is a point on the sheet, then the point (x,y,z) in space is reached by moving to (x,y) and then rising a distance z above the paper (points below it have negative z).
Very simple and clear, once a decision is made on which side of the sheet z is positive. By common agreement the positive branches of the (x,y, z) axes, in that order, follow the thumb and the first two fingers of the right hand when extended in a way that they make the largest angles with each other.
What follows uses the trigonometric functions sine and cosine; if these are not familiar to you, either skip the rest of the section, or go learn about them.
Polar Coordinates
![[Image:(r,phi)]](Sfigs/Spolar.gif)
Cartesian c oordinates (x,y) are not the only way of labeling a point P on a flat plane by a pair of numbers. Other ways exist, and they can be more useful in special situations.
One system ("polar coordinates") uses the length r of the line OP from the origin to P (i. e. the distance from P to the origin) and the angle that line makes with the x-axis. Angles are often denoted by Greek letters, and here we follow conventions by marking it with φ (Greek f). Note that while in the cartesian system x and y play very similar roles, here roles are divided: r gives distance and φ direction.
The two representations are closely related. From the definitions of the sine and cosine
x = r cos φ
y = r sin φ
That allows (x,y) to be derived from polar coordinates. To go in the opposite direction and derive (r,φ) from (x,y), note that from the above equations (or from the theorem of Pythagoras) one can derive r:
r2 = x2 + y2
Once r is known, the rest is easy
cos φ = x/r
sin φ = y/r
These relations fail only at the origin, where x = y = r = 0. At that point, φis undefined and one can choose for it whatever one pleases.
In three dimensional space, the cartesian labeling (x,y,z) is nicely symmetric, but sometimes it is convenient to follow the style of polar coordinates and label distance and direction separately. Distance is easy: you take the line OP from the origin to the point and measure its length r. You can even show from the theorem of Pythagoras that in this case
r2 = x2 + y2 + z2
All the points with the same value of r form a sphere of radius r around the origin O. On a sphere we can label each point by latitude λ (lambda, small Greek L) and longitude φ (phi, small Greek F), so that the position of any point in space could defined by the 3 numbers (r, λ, φ).
Azimuth and Elevation
 |
An old surveyor's tele-
scope (theodolite). |
The surveyor's telescope is designed to measure two such angles. The angle φ is measured counterclockwise in a horizontal plane, but surveyors (and soldiers) work with azimuth, a similar angle measured clockwise from north. Thus the directions (north, east, south, west) have azimuth (0°, 90°, 180°, 270°). A rotating table allows the telescope to be pointed in any azimuth.
The angle λ is called elevation and is the angle by which the telescope is lifted above the horizontal (if it looks down, λ is negative). The two angles together can in principle specify any direction: φ ranges from 0 to 360°, and λ from –90° (straight down or "nadir") to +90° (straight up or "zenith").
Again, one needs to decide from what direction is the azimuth measured--that is, where is azimuth zero? The rotation of the heavens (and the fact most humanity lives north of the equator) suggests (for surveyor-type measurements) the northward direction, and this is indeed the usual zero point. The azimuth angle (viewed from the north) is measured counterclockwise.
Mathematicians however prefer their own notation and replace "latitude" (or elevation) λ with co-latitude θ= 90 – λ deg., the angle not to the horizon but to the vertical. The angle θ (theta, one of two t-s in Greek) goes from 0 to 180°, not from –90° to + 90°. This actually may make more sense, because it is easier to measure an angle between two lines (OP and the vertical) rather than between a line and a flat plane (OP and the horizontal).]
[And in case you have to know: In 3 dimensions, when deriving the spherical coordinates (r, θ, φ) that correspond to cartesian (x,y,z) from the same origin, θ is measured from the +z-axis and φ is measured in the (x,y) plane, counterclockwise from the x-axis as seen from the +z side. This needs to be said, because viewed from –z ("from below") clockwise becomes counterclockwise, and vice versa.]
Teachers using this web page will find a related lesson plan at Lcelcoor.htm
It belongs to a set of lesson plans whose home page is at Lintro.htm.
Questions from Users:
***
Drawing a Perpendicular Line in Rectangular Coordinates
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Author and Curator: Dr. David P. Stern
Mail to Dr.Stern: stargaze("at" symbol)phy6.org .
Last updated: 10 October 2016
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