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Linear Algebra, Theory And Applications, 2012a

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2.7. EXERCISES 71<br />

this will suffice to explain the above question. Then the acceleration observed by a person<br />

on the earth relative to the apparently fixed vectors, i, k, j, is<br />

a B = −a (r B )(xi+yj+zk) − 2ω [−y ′ cos (φ) i+(x ′ cos (φ)+z ′ sin (φ)) j− (y ′ sin (φ) k)]<br />

Therefore, one obtains some differential equations from a B = x ′′ i + y ′′ j + z ′′ k by matching<br />

the components. These are<br />

x ′′ + a (r B ) x = 2ωy ′ cos φ<br />

y ′′ + a (r B ) y = −2ωx ′ cos φ − 2ωz ′ sin (φ)<br />

z ′′ + a (r B ) z = 2ωy ′ sin φ<br />

Now remember, the vectors, i, j, k are fixed relative to the earth and so are constant vectors.<br />

Therefore, from the properties of the determinant and the above differential equations,<br />

′<br />

(r ′ B × r B ) ′ i j k<br />

i j k<br />

=<br />

x ′ y ′ z ′<br />

=<br />

x ′′ y ′′ z ′′<br />

∣ x y z ∣ ∣ x y z ∣<br />

i j k<br />

=<br />

−a (r B ) x +2ωy ′ cos φ −a (r B ) y − 2ωx ′ cos φ − 2ωz ′ sin (φ) −a (r B ) z +2ωy ′ sin φ<br />

∣<br />

x y z ∣<br />

Then the k th component of this cross product equals<br />

ω cos (φ) ( y 2 + x 2) ′<br />

+2ωxz ′ sin (φ) .<br />

The first term will be negative because it is assumed p (t) is the location of low pressure<br />

causing y 2 +x 2 to be a decreasing function. If it is assumed there is not a substantial motion<br />

in the k direction, so that z is fairly constant and the last term can be neglected, then the<br />

k th component of (r ′ B × r B) ′ is negative provided φ ∈ ( 0, π 2<br />

)<br />

and positive if φ ∈<br />

( π<br />

2 ,π) .<br />

Beginning with a point at rest, this implies r ′ B × r B = 0 initially and then the above implies<br />

its k th component is negative in the upper hemisphere when φπ/2. Using the right hand and the geometric definition of the<br />

cross product, this shows clockwise rotation in the lower hemisphere and counter clockwise<br />

rotation in the upper hemisphere.<br />

Note also that as φ gets close to π/2 near the equator, the above reasoning tends to<br />

break down because cos (φ) becomes close to zero. Therefore, the motion towards the low<br />

pressure has to be more pronounced in comparison with the motion in the k direction in<br />

order to draw this conclusion.<br />

2.7 Exercises<br />

1. Show the map T : R n → R m defined by T (x) =Ax where A is an m × n matrix and<br />

x is an m × 1 column vector is a linear transformation.<br />

2. Find the matrix for the linear transformation which rotates every vector in R 2 through<br />

an angle of π/3.<br />

3. Find the matrix for the linear transformation which rotates every vector in R 2 through<br />

an angle of π/4.<br />

4. Find the matrix for the linear transformation which rotates every vector in R 2 through<br />

an angle of −π/3.

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