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During my lectures i've seen that in a case of a man swimming across a river in it's shortest path; my teacher had represented the direction of velocity in those cases and he had represented the length oppositte to the angle made by the direction to which the velocity has to be applied and the width of the river as the velocity of the river. Even after a wild run of thinking i still havent managed to know why he has taken the length oppositte to the angle as the velocity of the river.., could you please explain how?

Rasal V , 12 Years ago
Grade 12
anser 1 Answers
Askiitians Tutor Team

Last Activity: 5 Months ago

When analyzing the scenario of a man swimming across a river, we often break down the motion into components to understand how the swimmer's velocity interacts with the river's current. Your teacher's representation likely involves using vector components to illustrate this interaction. Let’s delve into this concept step by step.

Understanding Velocity Components

In physics, velocity is a vector quantity, which means it has both magnitude and direction. When a swimmer attempts to cross a river, two main velocities come into play:

  • The swimmer's velocity (Vs): This is the speed and direction in which the swimmer is moving relative to the water.
  • The river's velocity (Vr): This is the speed and direction of the river's current.

Breaking Down the Motion

To analyze the swimmer's path, we can visualize the situation using a right triangle. Here’s how it works:

  • The width of the river represents one side of the triangle.
  • The swimmer's velocity can be broken down into two components: one that moves directly across the river (perpendicular to the current) and another that is influenced by the river's current.
  • The river's velocity acts parallel to the riverbank, pushing the swimmer downstream.

Why the Opposite Length?

Your teacher likely referred to the length opposite the angle as the velocity of the river because of how we define angles in right triangles. In this context:

  • The angle formed between the swimmer's direction and the riverbank is crucial for determining how much of the swimmer's velocity is directed across the river versus downstream.
  • The opposite side of the angle corresponds to the component of the swimmer's velocity that is affected by the river's current.

Visualizing the Scenario

Imagine the swimmer is trying to swim directly across the river but is also being pushed downstream by the current. If we denote the angle between the swimmer's direction and the straight path across the river as θ, we can use trigonometric functions to analyze the situation:

  • The component of the swimmer's velocity that goes across the river can be calculated using the cosine function: Vs * cos(θ).
  • The component that is affected by the river's current can be calculated using the sine function: Vs * sin(θ).

In this case, the river's velocity (Vr) is represented by the length opposite to the angle because it shows how much of the swimmer's effort is being countered by the current, effectively pushing him downstream.

Example for Clarity

Let’s say the swimmer can swim at a speed of 2 m/s at an angle of 30 degrees to the riverbank. The river flows at 1 m/s. We can calculate the components:

  • Across the river: Vs * cos(30°) = 2 * √3/2 ≈ 1.73 m/s
  • Downstream due to the current: Vr = 1 m/s

In this example, the swimmer's effective path will be a combination of these two velocities, resulting in a diagonal path across the river. The angle and the lengths help visualize how the swimmer's effort is split between moving across the river and being pushed downstream.

Final Thoughts

Understanding the relationship between the swimmer's velocity and the river's current through vector components allows us to predict the swimmer's actual path. By using trigonometric functions, we can effectively analyze how much of the swimmer's effort is directed across the river versus being affected by the current. This approach not only clarifies the concept but also enhances our problem-solving skills in physics.

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