where C is traversed in the clockwise direction, r 5 èuè =h, sin u; cos ui; u ë0; çè; è6è where C is traversed in the counterclockwise direction èhow

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1 1 A Note on Parametrization The key to parametrizartion is to realize that the goal of this method is to describe the location of all points on a geometric object, a curve, a surface, or a region. This description must be one-to-one and onto: every point must be described once and only once. 1 Parametrization of Curves in R Let us begin with parametrizing the curve C whose equation is given by x + y =4 è1è i.e., a circle of radius centered at the origin. We start by associating a position vector r to each point èx; yè onc through the relation r = hx; yi: èè The coordinates x and y in èèare not arbitrary í they are related through equation è1è. This means that we are free to assign a value to only one of the coordinates of a typical point on C; the other coordinate must be determined from the equation of the circle. For this reason we say C has one degree of freedom. Choosing x as the parameter for C, we see from è1è that y = æp 4, x ; where the positive square root describes those points on C that lie above the x-axis and the negative square root the points below the x-axis. The complete parametrization of C is r 1 èxè =hx;p 4, x i and r èxè =hx;,p 4, x i; è3è where, ç x ç for r 1 and, x for r. Note that the points è,; 0è and è; 0è are arbitrarily assigned to r 1. We can now use the parametrization of C to determine tangent vectors to C, plot C on a graphics software, or to perform a line integral around C. Although the paramerization in è3è is adequate for the purpose of describing C, it is not the most convenient description of this curve. A more eæcient way to view C is to use polar coordinates to describe its points: x = cos ç; y = sin ç, with ç ë0; çè. So C can also be parametrized as r 3 èçè =h cos ç; sin çi; ç ë0; çè: è4è Note that r 3 in è4è does the job of both r 1 and r in è3è. The parametrizations r 1, r and r 3 are just a few ways out of the inænitely many ways that one could describe C. Here are three other parametrizations of the same curve: r 4 ètè =h sin t; cos ti; t ë0; çè; è5è

2 where C is traversed in the clockwise direction, r 5 èuè =h, sin u; cos ui; u ë0; çè; è6è where C is traversed in the counterclockwise direction èhow is r 5 diæerent from r 3?è and r 6 èwè =h sin w; cos wi; w ë0;çè: è7è To understand the diæerence between r 4 and r 6, compute the speed of a particle traveling around C according to these parametrizations. Let us now consider parametrizations of other familiar curves. Any two dimensional curve whose equation is given by y = fèxè can be parametrized as rèxè =hx; fèxèi; x èa; bè; èè so, for instance, the straight line y = mx + b can be viewed as rèxè = hx; mx + bi: è9è The circle of radius a centered at èb; cè is parametrized as rèçè =hb + a cos ç; c + a sin çi; ç è0; çë: è10è The ellipse whose equation is given by a x + b y = c is parametrized as èto see where the following expressions come from, divide a x + b y = c by c and set the term containing x equal to cos t and the one containing y to sin tè rètè =h c a cos t; c sin ti t è0; çè: è11è b Parametrization of Curves in R 3 Similar to curves in R, curves in R 3 still have only one degree of freedom, that is, a single parameter is suæcient to describe the coordinates of a typical point on curves in R 3. As an example, consider the straight line C that connects the two points P =è1; ; 1è and Q =è,1; 1; 3è. Let P = h1; ; 1i and Q = h,1; 1; 3i. Deæne v = Q, P = h,;,1; i. Note that v is parallel to the line C. So every point S on C can be accessed by the vector S = P + tv for some t R. So rètè =h1; ; 1i + th,;,1; i; t R è1è is a parametrization of C. In terms of coordinates, è1è is equivalent to : xètè = 1, t yètè =, t zètè = 1+t è13è

3 3 Every straight line C, whether in R or R 3, can be parametrized as rètè =r 0 + tv; t R è14è where r 0 is the position vector corresponding to a known point onc èsuch as h1; ; 1i in our previous exampleè, and v is a vector parallel to C. For instance, to ænd the parametrization of the line of intersection between the two planes x, 3y + z = and x + y + z = 0, ærst we ænd a point on this line by setting z = 0 in the equations of the planes and then solve for x and y to see that è 5 ;, ; 0è lies on C. Next, we note that 5 the vectors n 1 = h;,3; 1i and n = h1; 1; 1i are normal to the planes. Therefore, is parallel to C. Therefore v = n 1 æ n = h,4;,1; 5i rètè =h 5 ;, ; 0i + th,4;,1; 5i 5 è15è is a parametrization of C. More complicated curves are parametrized similarly. Typical points on a curve C are accessed by a position vector r of the form rètè =hxètè;yètè;zètèi: For example, the parametrization hsin t; cos t; ti describes a helix in R 3. Or the intersection of the plane x + y + z = 1 and the cylinder x + y = 1 is given by rètè =hcos t; sin t; 1, cos t, sin ti; t è0; çë: è16è 3 Parametrization of Surfaces Surfaces in R 3 are characterized by two degrees of freedom; one is allowed to vary two parameters independently to cover all points on a surface. The simplest examples are surfaces that are graphs of functions f that depend on two variables, z = fèx; yè. Such surfaces are often parametrized as rèx; yè =hx; y; fèx; yèi; axb; cyd: è17è For example, the surface z = x + y over the unit square is parametrized as rèx; yè =hx; y; x + y i; 0 x1; 0 y1: è1è The cylinder x + y = 1 is parametrized as rèç; zè =hcos ç; sin ç; zi; ç è0; çë; z R; è19è while the cylinder x + z = 4 is parametrized as rèç; yè =h cos ç; y; sin çi; ç è0; çë; y R; è0è

4 4 The surface of the disk of radius a in the plane z = b centered at the origin is given by rèu; vè =hu cos v; u sin v; bi; u ë0; 1ë; v è0; çë: è1è Certain surfaces are best parametrized in spherical coordinates where : x = ç cos ç sin ç; y = ç sin ç sin ç; z = ç cos ç: èè For example, the cone z = x + y can be parametrized as rèç; çè = p hç cos ç; ç sin ç; çi; ç R; ç è0; çë: è3è Similarly, the northern hemisphere of radius 3 centered at the origin may be parametrized as rèç; çè =3hcos ç sin ç; sin ç sin ç; cos çi; ç è0; çë; ç ë0; ç ë: è4è An alternative way of parametrizing this surface is as follows: q rèx; yè =3hx; y; 9, x, y i; x + y ç 9: è5è The boundary of this surface èthe circle of radius 3 in the xy-plane and centered at the originè is best parametrized using è4è by setting ç = ç in that relation to get rèçè = 3hcos ç; sin ç; 0i; ç è0; çë: è6è Once a parametrization rèu; vè of a surface S is known, the vector deænes a normal vector to S. r u æ r v 4 Parametrization of Regions in R 3 Regions in R 3 have three degrees of freedom. They are parametrized by rèu; v; wè where u, v and w take onvalues in respective intervals. For example, the region bounded by the cylinder x + y = 1 and the planes z =, and z = 1 is paramterized as rèr;ç;zè=hr cos ç; r sin ç; zi; 0 ç r ç 1; 0 ç ç ç ç;, ç z ç 1: è7è The boundary of this region consists of three surfaces S 1, S and S 3 given by : S 1 : r 1 èu; vè = hu cos v; u sin v;,i; 0 ç u ç 1; 0 ç vç; S : r èu; vè = hu cos v; u sin v; 1i; 0 ç u ç 1; 0 ç vç; S 3 : r 3 èu; vè = hcos v; sin v; ui;, ç u ç 1; 0 ç v:ç: èè

5 5 Similarly, the region inside the northern hemisphere of radius is parametrized as follows: rèç; ç; çè =hç cos ç sin ç; ç sin ç sin ç; ç cos çi; 0 ç ç ç ; 0 ç çç; 0 ç ç ç ç è9è The boundary of this region consists of two surfaces S 1 and S given by è S 1 : r 1 èç; çè = hcos ç sin ç; sin ç sin ç; cos çi; 0 ç çç; 0 ç ç ç ; S : r èr;çè = hr cos ç; r sin ç; 0i; 0 ç r ç ; 0 ç çç: è30è

Math 241: Calculus III Final Exam è300 points totalè Show All Work Name This test consists of 2 parts. There are 10 problems in Part I, each worth 18

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