Problem 9
Question
If a projectile is fired due east from a point on the surface of Earth at a northern latitude \(\lambda\) with a velocity of magnitude \(V_{0}\) and at an angle of inclination to the horizontal of \(\alpha,\) show that the lateral deflection when the projectile strikes Earth is $$ d=\frac{4 V_{0}^{3}}{g^{2}} \cdot \omega \sin \lambda \cdot \sin ^{2} \alpha \cos \alpha $$ where \(\omega\) is the rotation frequency of Earth.
Step-by-Step Solution
Verified Answer
In order to find the lateral deflection, we first decomposed the initial velocity into horizontal and vertical components, then calculated the time of flight and the horizontal displacement. Afterward, we determined the Coriolis acceleration and integrated it over the time of flight to find the lateral deflection. Finally, we obtained the formula for the lateral deflection of the projectile as follows:
$$
d=\frac{4 V_{0}^{3}}{g^{2}} \cdot \omega \sin \lambda \cdot \sin ^{2} \alpha \cos \alpha
$$
1Step 1: Decompose the initial velocity into components
We first need to find the components of the initial velocity \(V_0\) in the horizontal (eastward) and vertical (upward) directions. This can be done using trigonometric functions:
- Horizontal component: \(V_x = V_0 \cos \alpha\)
- Vertical component: \(V_y = V_0 \sin \alpha\)
2Step 2: Calculate the time of flight
Using the vertical component of velocity \(V_y\), we can find the time of flight \(t_f\) when the projectile strikes the Earth. At maximum height, vertical velocity becomes zero, and the time to reach maximum height is:
$$ t_h = \frac{V_y}{g} $$
Since the projectile takes equal time to ascend and descend, the time of flight is:
$$ t_f = 2t_h = \frac{2V_y}{g} = \frac{2V_0 \sin \alpha}{g} $$
3Step 3: Calculate the horizontal displacement
We will now calculate the horizontal displacement \(x_f\) of the projectile using the horizontal component of velocity \(V_x\) and time of flight \(t_f\):
$$ x_f = V_x \cdot t_f = V_0 \cos \alpha \cdot \frac{2V_0 \sin \alpha}{g} $$
4Step 4: Calculate the Coriolis acceleration
The projectile experiences Coriolis acceleration due to Earth's rotation. This acceleration can be determined by the following formula:
$$ a_c = 2 \omega v_y \sin \lambda $$
5Step 5: Calculate the lateral deflection
To find the lateral deflection \(d\), we will integrate the Coriolis acceleration \(a_c\) over the time of flight \(t_f\). We have:
$$ d = \int_0^{t_f} a_c\: dt = \int_0^{t_f} 2 \omega v_y \sin \lambda\: dt $$
Now we integrate by substitution. Let \(u = v_y = V_0 \sin \alpha - gt\). Then,
$$ du = -g\: dt $$
and
$$ dt = -\frac{1}{g}du $$
And our integral becomes:
$$ d = \int_{V_0 \sin \alpha}^0 2 \omega u \sin \lambda \left( -\frac{1}{g} du \right) = \frac{2\omega \sin \lambda}{g} \int_{V_0 \sin \alpha}^0 u\: du $$
Now integrate and evaluate the definite integral:
$$ d = \frac{2\omega \sin \lambda}{g} \left[ \frac{u^2}{2} \right]_{V_0 \sin \alpha}^0 = -\frac{2\omega \sin \lambda}{g} \left(\frac{1}{2} (V_0 \sin \alpha)^2 \right) $$
Multiply this result by the horizontal displacement \(x_f\) from Step 3:
$$ d = -\left(\frac{2\omega \sin \lambda}{g} \right) \cdot \frac{1}{2} (V_0 \sin \alpha)^2 \cdot V_0 \cos \alpha \cdot \frac{2V_0 \sin \alpha}{g} $$
Simplifying gives the desired result:
$$ d=\frac{4 V_{0}^{3}}{g^{2}} \cdot \omega \sin \lambda \cdot \sin ^{2} \alpha \cos \alpha $$
Key Concepts
Projectile MotionEarth's RotationLateral DeflectionTrigonometric Decomposition
Projectile Motion
Projectile motion refers to the path that an object follows when it is launched into the air. This motion is typically divided into two components: horizontal and vertical. Understanding these components is crucial for solving problems related to projectile motion.
Here's how it works:
Here's how it works:
- The **horizontal component** is concerned with the constant velocity at which the projectile moves eastward. It does not change since there's no external horizontal force acting on it once airborne (ignoring air resistance).
- The **vertical component** deals with the upward force and is subject to gravity, which pulls the projectile back down.
Earth's Rotation
Earth's rotation greatly affects projectile motion, especially over long distances. This rotation causes the Coriolis Effect, an apparent deflection of the motion of objects moving over Earth's surface.
Here's why it matters:
Here's why it matters:
- As Earth rotates from west to east, any projectile motion needs to account for this rotation.
- This rotation results in different speeds of surface movement depending on latitude. Near the equator, the rotational speed is higher than at the poles.
Lateral Deflection
Lateral deflection refers to the shift of a projectile’s path due to Earth's rotation.
Here's the truth about lateral deflection:
Here's the truth about lateral deflection:
- It is the sideways or lateral shift in a projectile’s path, caused by the Coriolis Effect.
- This deflection occurs to the right in the northern hemisphere and to the left in the southern hemisphere.
Trigonometric Decomposition
Trigonometric decomposition involves breaking down vector quantities into smaller components using trigonometry. In projectile motion, it's used to decompose the initial velocity into horizontal and vertical components.
Here's how you do it:
Here's how you do it:
- **Horizontal Component**: Use \( V_x = V_0 \cos \alpha \). This component moves the projectile eastward.
- **Vertical Component**: Use \( V_y = V_0 \sin \alpha \). This component allows the projectile to ascend and later descend.
Other exercises in this chapter
Problem 5
Perform a numerical calculation using the parameters in Example 10.2 and Figure \(10-4 \mathrm{e},\) but find the initial velocity for which the path of motion
View solution Problem 8
If a particle is projected vertically upward to a height \(h\) above a point on Earth's surface at a northern latitude \(\lambda\), show that it strikes the gro
View solution Problem 11
Obtain an expression for the angular deviation of a particle projected from the North Pole in a path that lies close to Earth. Is the deviation significant for
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Show that the small angular deviation \(\varepsilon\) of a plumb line from the true vertical (i.e. toward the center of Earth) at a point on Earth's surface at
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