Question map
Consider the following statements : 1. The winds which blow between 30° N and 60° S latitudes throughout the year are known as westerlies. 2. The moist air masses that cause winter rains in North-Western region of India are part of westerlies. Which of the statements given above is/are correct?
Explanation
**Statement 1 is incorrect.** Westerlies are prevailing winds that blow from the west at midlatitudes.[1] The statement claims westerlies blow between 30° N and 60° S, which is geographically impossible as it spans both hemispheres. Westerlies typically blow between approximately 30° and 60° latitude in *each* hemisphere (30°-60° N and 30°-60° S separately), not across hemispheres.
**Statement 2 is correct.** In north-western region of the subcontinent, winter precipitation is caused by the depressions that are associated with the westerly disturbances moving out from the Mediterranean Sea.[2] The western disturbances are the low pressure depressions which originate from the Mediterranean Sea and enter India after crossing Turkey, Syria, Iraq, Iran, Afghanistan and Pakistan. The jet streams plays an important role in bringing the western disturbances to India.[3] These disturbances are indeed part of the westerly wind system that brings winter rainfall to northwestern India.
Therefore, only statement 2 is correct, making option B the right answer.
Sources- [1] https://education.nationalgeographic.org/resource/wind/
- [2] Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 4: Climate of India > 1. The Cold Weather Season > p. 18
- [3] Environment and Ecology, Majid Hussain (Access publishing 3rd ed.) > Chapter 8: Natural Hazards and Disaster Management > Western Disturbances > p. 52
PROVENANCE & STUDY PATTERN
Full viewStatement 1 is a classic 'Coordinate Trap'—the numbers (30, 60) are correct, but the span (N to S) implies a wind blowing across the Equator, which defies physics (Trade Winds exist there). Statement 2 is a direct lift from NCERT Class XI (Indian Physical Environment). Strategy: Visualize the globe, don't just read the text.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
- Defines westerlies as prevailing winds that blow from the west at midlatitudes, indicating a latitude-band location rather than a single hemisphere-spanning band.
- Implies westerlies occupy the midlatitude zones (between horse latitudes and polar easterlies), not specifically a continuous band from 30° N to 60° S.
- Gives the approximate latitude of the horse latitudes (~30–35° N and S), which serve as the equatorward boundary for midlatitude wind zones.
- Shows westerlies lie poleward of roughly 30° (not extending as a single band from 30° N across the equator to 60° S).
- Provides an example of strong westerly winds affecting the Falkland Islands (a Southern Hemisphere midlatitude location), supporting that westerlies occur in midlatitudes of both hemispheres.
- Implies westerlies are characteristic of midlatitude regions (e.g., around 50°S), not a continuous 30°N–60°S band throughout the year.
Defines 'prevailing winds' as winds that blow almost in the same direction throughout the year and explicitly lists westerly winds as one of the major prevailing/planetary winds.
A student can combine this with latitude bands for 'prevailing' cells (e.g., Ferrel cell) to judge whether westerlies should be year-round in a given latitude band.
Links westerlies to the Ferrel cell and places them in the 'middle latitudes' (the circulation between subtropical highs and polar lows).
Knowing Ferrel cell occupies mid-latitudes, a student can map the Ferrel cell approximate limits against 30°–60° to assess the statement's latitudinal claim.
Gives a best-developed latitude range for southern hemisphere westerlies (40°–65° S) and notes the poleward boundary is highly fluctuating; contrasts stronger southern vs irregular northern westerlies.
Using these ranges and the noted fluctuation, a student could question the uniform 30°–60° N/S band and year-round persistence implied by the statement.
States that not all western coasts of the temperate zone receive Westerlies throughout the year, and gives examples where westerlies are seasonal.
A student could use these examples to infer that westerlies are not uniformly year-round everywhere within a broad latitude belt, challenging the 'throughout the year' claim.
Explains that upper-level jet streams are 'westerlies' flowing west to east in both hemispheres, indicating a vertical/altitude component and hemispheric symmetry.
A student might combine surface vs upper-level distinctions with latitude info to test whether the term 'westerlies' uniformly applies at surface across the stated band year-round.
- Explicitly identifies winter precipitation in NW India as caused by depressions associated with 'westerly disturbances'.
- States these disturbances move out from the Mediterranean Sea toward India, linking their origin and path to mid-latitude westerly systems.
- Describes the low-pressure systems (western disturbances) originating over the Mediterranean/western Asia and moving into India 'along with the westerly flow'.
- Directly connects these depressions' movement into India with the westerly circulation.
- Defines western disturbances as low-pressure depressions originating in the Mediterranean and notes the jet stream's role in bringing them to India.
- Links these disturbances to light winter rains beneficial to Rabi crops, reinforcing their climatic impact as part of the westerly-related systems.
- [THE VERDICT]: Mixed Bag. Statement 1 is a 'Geography Logic Trap' (GC Leong Ch 14). Statement 2 is a 'Sitter' (NCERT Class XI, Ch 4).
- [THE CONCEPTUAL TRIGGER]: Planetary Wind Systems (General Geography) intersecting with Indian Climate (Winter Season).
- [THE HORIZONTAL EXPANSION]: Memorize the specific belts: Doldrums (5°N-5°S), Trade Winds (5°-30°), Horse Latitudes (30°-35°), Westerlies (35°-60°), Polar Easterlies (65°-90°). Also, link 'Western Disturbances' to the Subtropical Westerly Jet Stream (STWJ).
- [THE STRATEGIC METACOGNITION]: When you see coordinates like '30° N to 60° S', pause and draw a mental line. Does one wind system cover the Northern Hemisphere, Equator, and Southern Hemisphere? Impossible due to Coriolis force and pressure belts. This was a test of visualization, not just definition.
References identify westerlies as one of the major prevailing/planetary winds and associate them with mid‑latitude (Ferrel) circulation.
High-yield for UPSC geography: questions often ask definitions of planetary wind systems and their relation to atmospheric cells. Mastering this links to pressure belts, mid‑latitude climate, and jet stream dynamics; learn definitions and Ferrel cell mechanics with diagrammatic revision.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 23: Pressure Systems and Wind System > Primary winds or Prevailing Winds or Planetary Winds > p. 318
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 23: Pressure Systems and Wind System > Ferrel Cell > p. 317
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 27: Jet streams > Upper Tropospheric Westerlies > p. 385
Evidence highlights the westerlies' prominent band (e.g., 40°–65° S) and the nomenclature Roaring Forties/Furious Fifties used for southern latitudes.
Frequently tested: UPSC often asks latitude ranges and hemisphere contrasts. Knowing the typical latitudinal bands and stronger southern persistence helps eliminate wrong options in MCQs and supports answers on oceanic/storm patterns; memorise ranges from sources and note exceptions.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 23: Pressure Systems and Wind System > The Westerlies > p. 319
- Certificate Physical and Human Geography , GC Leong (Oxford University press 3rd ed.) > Chapter 14: Climate > Pressure and Planetary Winds > p. 140
References show westerlies vary by hemisphere and region (southern stronger/persistent, northern more irregular) and that some coasts receive westerlies only seasonally (e.g., winter).
Important for applied questions on regional climates, coastal rainfall and cyclone behaviour. UPSC may ask about seasonal influence on western coasts or interaction with tropical cyclones; study regional examples and seasonal shifts rather than assuming year‑round uniformity.
- Certificate Physical and Human Geography , GC Leong (Oxford University press 3rd ed.) > Chapter 14: Climate > Pressure and Planetary Winds > p. 140
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 23: Pressure Systems and Wind System > The Westerlies > p. 319
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 26: Tropical Cyclones > 26.4. Path of Tropical Cyclones > p. 371
The references repeatedly identify western disturbances as temperate depressions originating over the Mediterranean and causing NW India's winter rains.
High-yield for climate questions: explains a major source of winter precipitation in India and links to agriculture (Rabi crops) and Himalayan snowfall. Master by mapping origin → path → surface impacts and practising linked MCQs and diagram-based questions.
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 4: Climate of India > 1. The Cold Weather Season > p. 18
- Environment and Ecology, Majid Hussain (Access publishing 3rd ed.) > Chapter 8: Natural Hazards and Disaster Management > Western Disturbances > p. 52
Several references state that upper-air westerly jet streams steer these depressions into India.
Important for understanding dynamic causes of weather systems and seasonality; connects to atmospheric circulation, cyclone tracks and seasonal rainfall patterns. Learn by studying jet stream location/seasonal shifts and their effects on surface weather.
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 4: Climate of India > JET STREAM AND INDIAN MONSOON > p. 8
- INDIA PHYSICAL ENVIRONMENT, Geography Class XI (NCERT 2025 ed.) > Chapter 4: Climate > Understanding the Monsoon > p. 33
Evidence notes that the middle-latitude westerlies (westerly flow) extend southward and carry depressions into north India causing winter precipitation.
Useful for questions contrasting monsoon (tropical) systems with temperate westerlies; helps answer why NW India gets winter rains while most of India is dry. Prepare by comparing latitude-linked wind belts and their seasonal shifts.
- Geography of India ,Majid Husain, (McGrawHill 9th ed.) > Chapter 4: Climate of India > 1. The Cold Weather Season > p. 17
- CONTEMPORARY INDIA-I ,Geography, Class IX . NCERT(Revised ed 2025) > Chapter 4: Climate > The Cold Weather Season (Winter) > p. 28
The 'Easterly Jet Stream'. While the Westerly Jet brings winter rain (Western Disturbances), the Tropical Easterly Jet (TEJ) is unique to the Asian Summer Monsoon and is crucial for the onset of the South-West Monsoon. UPSC loves contrasting these two jets.
Apply the 'Equator Test'. Statement 1 says Westerlies blow from 30°N to 60°S. This range includes the Equator (0°). You know Trade Winds blow near the equator. Therefore, a single wind system cannot span this entire range. Statement 1 is physically impossible. Eliminate A and C immediately.
Food Security & Economy: Western Disturbances are critical for India's 'Rabi' crop (Wheat). A failure of these westerlies leads to wheat inflation, linking physical geography directly to GS-3 Agriculture and Inflation dynamics.