Parametrization as Arc Length: Why Do We Need It?

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SUMMARY

The discussion centers on the importance of parametrization in terms of arc length for curves in both the plane and space. It highlights the convenience of using arc length as a parameter, particularly in real-life scenarios such as biking and hiking, where understanding elevation changes along a route is crucial. Key formulas for arc length are provided, including s = ∫√((dx/dt)² + (dy/dt)²) dt and s = ∫√((dy/dx)² + 1) dx. The conversation also emphasizes that parametrization allows for the identification of unit tangent vectors, enhancing geometric interpretations of curves.

PREREQUISITES
  • Understanding of calculus, specifically integration and differentiation.
  • Familiarity with parametric equations and their applications.
  • Knowledge of geometric concepts related to curves and tangents.
  • Basic comprehension of real-world applications in biking and hiking.
NEXT STEPS
  • Study the derivation and applications of arc length formulas in calculus.
  • Explore the concept of unit tangent vectors and their significance in geometry.
  • Investigate parametric equations and their role in representing complex curves.
  • Learn about the geometric interpretation of curves, including circles and their properties.
USEFUL FOR

Students studying calculus, mathematicians interested in geometric interpretations, and outdoor enthusiasts seeking to understand elevation changes along trails.

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Homework Statement



Our prof talked about arc length as a parameter today and I understand how to do problems associated with it, however I do not fully understand why we do it.

Homework Equations



In our text, the only relevant reading says: "A curve in the plane or in space can be parametrized in terms of the arc length s."


Would someone be able to give me a geometric interpretation on why we need to do this parametrization?

Thanks!
 
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It is often convenient. Biking and hiking give intuitive real-life examples. IF you hike trails in the mountains, or watch the Tour de France on TV, you'll see a graph of elevation as a function of distance along the route. It is useful to know, e.g., that a steep climb is coming up at mile 2.6 followed by a gentle descent for the next half mile, etc. It is far less convenient to have to look at a topo map that gives elevation at every x,y point (or latitude/longitude), because you have to painstakingly figure out what it is along the trail you'll be taking. Parametrization along the arc or curve or trail is the more appropriate and convenient way to work the problem.
 
You don't need to. It's often convenient, as marcusl said.

One formula for arclength is
s= \int \sqrt{\left(\frac{dx}{dt}\right)^2+ \left(\frac{dy}{dt}\right)^2}dt
where x and y are functions of some parameter t.

On the other hand if we just have y a function of x, we can use the formula
s= \int \sqrt{\left(\frac{dy}{dx}\right)^2+ 1}dx

Of course, there exist many interesting curves in which y is not a function of x! Example: the circle.
 
http://en.wikipedia.org/wiki/Unit_circle

y^2 + x^2=r^2 : function of a circle.

This is actually for wiki not a bad little guide to circles, interesting as it shows all the relationships to 0 the center of the circle and their angles, I just though I'd mention it as it is a good picture of how the angles relate and to which sides. The arc length is of course the distance along the circumference of the circle.

Probably not relevant, but interesting.

The curve \int_0^{ln 2}{\sqrt{1+e^{2x}}dx} => \frac {1}{2} \ln [\sqrt {(1+e^2x)}] - \frac {1}{2} \ln [\sqrt {(1+e^2x)}]+\sqrt {1+e^2x}+C
describes the volume of a toroidal too as I recently found out.

The definite integrals value is found by placing e as 2. As ln2(e)=2 in this case and then subtracting the lower limit.
 
Last edited:
great thanks a lot!
 
For some reason, in my first response I thought you were asking about calculating arc-length when a curve is given by parametric equations. Now I see that you are asking about using arclength as a parameter.

One point about parameterization in terms of arc length is that it is obvious[/t]! Choose any point at all to correspond to s= 0, choose one direction on the curve to be + and another to be -. Then just literally measure along the curve. The point at distance s from the starting point (in the positive direction) is labeled by parameter s, in the negative direction by parameter -s.

Another nice thing is that while the vector you get by differentiating the position vector with respect to any parameter is a tangent vector to the curve, if you use arclength, it is the unit tangent vector.
 

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