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With reference to "Coriolis force", which of the following statements is/are correct ? 1. It increases with increase in wind velocity. 2. It is maximum at the poles and is absent at the equator. Select the answer using the code given below :
Explanation
The correct answer is option C because both statements are correct.
The Coriolis force acting on a body increases with an increase in its velocity.[1] This relationship is also evident from the mathematical formula, where the magnitude (Coriolis force) of the effect is given by 2νω sin ϕ, in which ν is the velocity of the object, ω is the angular velocity of the Earth, and ϕ is the latitude.[2] Therefore, statement 1 is correct.
Regarding statement 2, the Coriolis force is zero at the equator but increases with latitude, reaching a maximum at the poles.[2] This is because at the equator, ϕ = 0° and at the poles, ϕ = 90°[2], and since the force depends on sin ϕ, it becomes zero at the equator (sin 0° = 0) and maximum at the poles (sin 90° = 1). Hence, statement 2 is also correct.
Since both statements accurately describe the characteristics of the Coriolis force, option C (Both 1 and 2) is the correct answer.
Sources- [1] Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 27: Jet streams > Geostrophic Wind > p. 384
- [2] Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 23: Pressure Systems and Wind System > Causes of The Coriolis Effect > p. 309
PROVENANCE & STUDY PATTERN
Guest previewThis is a classic 'Return on Investment' question directly from NCERT Class XI, Chapter 9. It proves that despite the hype around dynamic questions, static Climatology remains the backbone. If you missed this, you are neglecting the 'Forces Affecting Wind' section which is fundamental to understanding Cyclones and Jet Streams.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
- Gives the quantitative expression F_C = 2 ν ω sin φ, where ν is the object's velocity — directly showing proportionality to speed.
- Explicitly links the Coriolis magnitude to the motion of the object (wind) and latitude, making the velocity dependence central.
- Plainly states that the Coriolis force acting on a body increases with an increase in its velocity.
- Applies this to fast upper‑air winds (jet streams), showing practical cases where higher speeds produce larger Coriolis effects.
- States the deflection (Coriolis effect) increases with wind velocity and with latitude.
- Connects increased pressure gradient → higher wind speed → larger deflection, reinforcing the speed dependence.
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