27.09.2014 Views

Notes on Relativity and Cosmology - Physics Department, UCSB

Notes on Relativity and Cosmology - Physics Department, UCSB

Notes on Relativity and Cosmology - Physics Department, UCSB

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

4.3. MORE ON MINKOWSKIAN GEOMETRY 103<br />

Thus, it is still moving at a good fracti<strong>on</strong> of “the speed of light.” Anyway, if<br />

the water is also flowing (say, toward us) at a fast rate, then the speed of the<br />

light toward us is given by the above expressi<strong>on</strong> in which the velocities do not<br />

just add together. This is just what Fizeau found 5 , though he had no idea why<br />

it should be true!<br />

Now, the above formula looks like a mess. Why in the world should the compositi<strong>on</strong><br />

of two velocities be such an awful thing? As with many questi<strong>on</strong>s, the<br />

answer is that the awfulness is not in the compositi<strong>on</strong> rule itself, but in the filter<br />

(the noti<strong>on</strong> of velocity) through which we view it. We will now see that, when<br />

this filter is removed <strong>and</strong> we view it in terms native to Minkowskian geometry,<br />

the result is quite simple indeed.<br />

Recall the analogy between boosts <strong>and</strong> rotati<strong>on</strong>s. How do we describe rotati<strong>on</strong>s?<br />

We use an angle θ. Recall that rotati<strong>on</strong>s mix x <strong>and</strong> y through the sine <strong>and</strong> cosine<br />

functi<strong>on</strong>s.<br />

x 1= 0<br />

x = r sin θ 2<br />

r<br />

y = r cosθ<br />

2<br />

y 1= 0<br />

x 2 = r sin θ,<br />

y 2 = r cosθ. (4.5)<br />

Note what happens when rotati<strong>on</strong>s combine. Well, they add of course. Combining<br />

rotati<strong>on</strong>s by θ 1 <strong>and</strong> θ 2 yields a rotati<strong>on</strong> by an angle θ = θ 1 + θ 2 . But<br />

we often measure things in terms of the slope m = x y<br />

(note the similarity to<br />

v = x/t). Now, each rotati<strong>on</strong> θ 1 , θ 2 is associated with a slope m 1 = tanθ 1 ,<br />

m 2 = tanθ 2 . But the full rotati<strong>on</strong> by θ is associated with a slope:<br />

m = tanθ = tan(θ 1 + θ 2 )<br />

= tan θ 1 + tanθ 2<br />

1 − tan θ 1 tan θ 2<br />

= m 1 + m 2<br />

1 − m 1 m 2<br />

. (4.6)<br />

So, by expressing things in terms of the slope we have turned a simple additi<strong>on</strong><br />

rule into something much more complicated.<br />

5 Recall that Fizeau’s experiments were <strong>on</strong>e of the motivati<strong>on</strong>s for Michels<strong>on</strong> <strong>and</strong> Morely.<br />

Thus, we now underst<strong>and</strong> the results not <strong>on</strong>ly of Michels<strong>on</strong> <strong>and</strong> Morely’s experiment, but also<br />

of the experiments that prompted their work.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!