Question map
On 21st June, the Sun
Explanation
The correct answer is option A because on 21st June, the northern hemisphere is tilted towards the sun, and the rays of the sun fall directly on the Tropic of Cancer[1]. At the Arctic Circle, the Sun never 'sets' at mid-summer (21 June) and there is a complete 24-hour period of continuous daylight[2]. This phenomenon occurs because of the axial tilt of the Earth, the Sun does not set at high latitudes in local summer[3].
Option B is incorrect because on 21st June it is winter in the Southern Hemisphere, so the Antarctic Circle experiences polar night, not midnight sun. Option C is incorrect because the Sun is vertically overhead at the equator on two days each year, usually 21 March and 23 September[4] (the equinoxes), not on 21st June. Option D is incorrect because on 22nd December, the Tropic of Capricorn receives direct rays of the sun[5], not on 21st June when the sun is directly over the Tropic of Cancer.
Sources- [1] Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Summer Solstice > p. 252
- [2] Certificate Physical and Human Geography , GC Leong (Oxford University press 3rd ed.) > Chapter 2: The Earth's Crust > The Earth's Revolution > p. 7
- [3] Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Midnight Sun > p. 253
- [4] Certificate Physical and Human Geography , GC Leong (Oxford University press 3rd ed.) > Chapter 2: The Earth's Crust > THE ALTITUDE OF THE MIDDAY SUN > p. 7
- [5] Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Winter Solstice > p. 253
PROVENANCE & STUDY PATTERN
Full viewThis is a textbook 'Sitter' question found in the first 10 pages of any standard Geography resource (NCERT Class 6 or GC Leong). It tests the fundamental definition of the Summer Solstice. If you get this wrong, you are statistically out of the race because 95% of serious aspirants will mark this correctly in under 30 seconds.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
- Statement 1: On 21st June, does the Sun remain above the horizon (midnight sun) at the Arctic Circle?
- Statement 2: On 21st June, does the Sun remain above the horizon (midnight sun) at the Antarctic Circle?
- Statement 3: On 21st June, is the Sun directly overhead (at zenith) at local noon on the Equator?
- Statement 4: On 21st June, is the Sun directly overhead (at zenith) at local noon on the Tropic of Capricorn?
- Explains that due to Earth's axial tilt the Sun does not set at high latitudes in local summer.
- Specifically states the Sun remains continuously visible for one day during the summer solstice at the polar circle (21st June).
- Explicitly asserts that at the Arctic Circle the Sun never sets at mid-summer (21 June) giving a complete 24-hour period of daylight.
- Presents the mid-summer/mid-winter symmetry that underpins polar day/night at polar circles.
- States that on 21st June the northern hemisphere is tilted towards the Sun and the whole Arctic region falls within the zone of illumination all day.
- Links the summer solstice geometry to the longest day and continuous daylight in Arctic latitudes.
- Specifies that continuous visibility at a polar circle occurs on the summer solstice and links the Northern solstice to 21 June and the Southern solstice to 22 December
- By distinguishing the solstice dates, it implies the Antarctic Circle's 24βhour sun occurs on 22 Dec, not 21 Jun
- Explains that on 21 June the northern hemisphere tilts toward the Sun and the entire Arctic falls within the zone of illumination
- States that conditions are reversed in the southern hemisphere, implying Antarctic Circle is not in continuous daylight on 21 June
- Explicitly says the Sun never sets at the Arctic Circle on 21 June (midβsummer) and that the southern hemisphere experiences the reverse
- Reversal implies the Antarctic Circle does not experience midnight sun on 21 June
- States when the Sun is directly overhead at the equator: only twice per year, at the two equinoxes.
- Lists the equinox dates (March 20 and September 22), which do not include June 21, implying June 21 is not a date when the Sun is overhead at the equator.
- Identifies June 21 (about) as the solstice when the Sun is directly above the Tropic of Cancer.
- If on June 21 the Sun is over the Tropic of Cancer, it is not directly overhead at the equator on that date.
- Confirms that at the equator the Sun is directly overhead at noon on the two equinoxes.
- Reinforces that the overhead dates for the equator are the equinoxes, not the June solstice.
States that on 21st June the sun's rays fall directly on the Tropic of Cancer (northern hemisphere tilted towards the sun).
A student can combine this with the basic fact that the Equator is distinct from the Tropic of Cancer to infer that the Equator would not receive the sun's direct vertical rays on that date.
Gives the general rule that the Sun is vertically overhead at the Equator on the equinoxes (around 21 March and 23 September).
Using this rule, a student can contrast equinox dates with 21 June to judge whether zenith passage at the Equator occurs on the solstice.
Explicitly notes that direct rays fall on the Equator on 21 March and 23 September (the equinoxes).
A student can use this pattern to exclude other dates (such as 21 June) for the Equator's zenith sun.
Describes how to calculate the midday Sun's elevation for a given place and date (worked example for 21 June).
A student could apply this method to the Equator for 21 June to determine whether the elevation equals 90Β° (zenith) or not.
Notes that at the Equator there is little difference in intensity of sunrays in different months and that day/night lengths are ~12 hours year-round.
A student might combine this with other rules (e.g., where direct rays fall on solstice) to reason about whether 'always similar' implies zenith on 21 June (it does not by itself).
- Explicitly links 21st June (summer solstice) with the Sun's rays falling directly on the Tropic of Cancer.
- Shows northern hemisphere tilt toward the Sun on 21st June, implying the zenith position is at the Tropic of Cancer rather than the Tropic of Capricorn.
- Specifies that the Tropic of Capricorn receives direct rays on 22nd December (winter solstice), not on 21st June.
- Provides the complementary date demonstrating that the Tropic of Capricorn is a December zenith location, contradicting a June zenith there.
- States that the Tropics mark the limits of the overhead Sun, so the zenith position shifts between the Tropic of Cancer and Tropic of Capricorn over the year.
- Notes equinox dates when the Sun is overhead at the Equator, framing the annual motion that places the Sun at the Tropic of Cancer in June and at the Tropic of Capricorn in December.
- [THE VERDICT]: Sitter. Direct hit from GC Leong Chapter 2 (The Earth's Revolution) or NCERT Class 6 (Motions of the Earth).
- [THE CONCEPTUAL TRIGGER]: Earth's Axial Tilt (23.5Β°) and Revolution. The specific geometry of the 'Circle of Illumination' relative to the poles on Solstice dates.
- [THE HORIZONTAL EXPANSION]: Memorize the 'Solar Calendar': June 21 (Cancer Zenith, Arctic Day), Dec 22 (Capricorn Zenith, Antarctic Day), March 21/Sept 23 (Equator Zenith). Also, link Perihelion (Jan 3) and Aphelion (July 4) to these datesβnote that Earth is actually farthest from the Sun during the Northern Summer.
- [THE STRATEGIC METACOGNITION]: Do not just memorize 'June 21 = Summer'. Visualize the tilt. If you cannot draw the Earth showing the North Pole tilted *towards* the Sun and the Circle of Illumination cutting *behind* the Arctic Circle, you have not understood the mechanism, only memorized the fact.
Axial tilt causes the northern hemisphere to face the Sun on 21 June, producing the longest day and continuous daylight at high northern latitudes.
High-yield for questions on seasons, solstices and day-length variations; connects to Earth's orientation, seasonal climate patterns and insolation distribution. Mastery helps answer questions on why seasons occur and spatial daylight contrasts between latitudes.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Midnight Sun > p. 253
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Summer Solstice > p. 252
The zone of illumination on the summer solstice includes the Arctic Circle, producing polar day (midnight sun) there.
Important for reasoning about which latitudes receive continuous daylight or darkness at key solar positions; useful for map-based and conceptual UPSC geography questions about polar phenomena and daylight duration.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Summer Solstice > p. 252
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Midnight Sun > p. 253
The Arctic Circle marks the latitude where a full 24-hour period of daylight occurs at mid-summer and full darkness at mid-winter.
Directly relevant to factual and conceptual questions asking what specific latitudinal lines signify (e.g., Arctic/Antarctic circles vs. tropics); helps eliminate distractors in objective questions and supports linked topics like polar climate and biomes.
- Certificate Physical and Human Geography , GC Leong (Oxford University press 3rd ed.) > Chapter 2: The Earth's Crust > The Earth's Revolution > p. 7
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Midnight Sun > p. 253
21 June is the northern summer solstice while 22 December is the southern summer solstice, so day/night patterns swap between hemispheres.
Highβyield for solving questions about which hemisphere or which polar circle experiences continuous daylight or darkness on a given date; links directly to seasonality, insolation patterns and latitude effects. Mastering this helps eliminate answer choices about polar day/night timing and connects to climatology and EarthβSun geometry.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Midnight Sun > p. 253
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Summer Solstice > p. 252
Polar circles experience a 24βhour day on their respective summer solstice rather than simultaneously on the same calendar date worldwide.
Frequently examined concept in physical geography questions on extreme day length, polar climates, and latitude thresholds; useful for reasoning about when polar day/night occur and for comparing Arctic vs Antarctic phenomena.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Midnight Sun > p. 253
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Midnight Sun > p. 254
Tilt of the Earth on solstice dates places the Arctic within continuous illumination on 21 June while the Antarctic is in the opposite condition.
Important for mapping day length variation with latitude and season; enables candidates to predict daylight/darkness outcomes for specific latitudes and dates, and links to questions on solar insolation, climate zones and seasonal contrasts.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Summer Solstice > p. 252
- Certificate Physical and Human Geography , GC Leong (Oxford University press 3rd ed.) > Chapter 2: The Earth's Crust > The Earth's Revolution > p. 7
The point where the Sun is directly overhead shifts seasonally and reaches the Tropic of Cancer around 21 June.
High-yield for questions on solar declination, seasons and sun-angle calculations; connects to topics on solstices, seasonal insolation patterns and latitudinal climate differences. Mastery helps answer which latitude receives vertical sun rays on specific dates and eliminates wrong latitude options.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 19: The Motions of The Earth and Their Effects > Summer Solstice > p. 252
- Certificate Physical and Human Geography , GC Leong (Oxford University press 3rd ed.) > Chapter 2: The Earth's Crust > THE ALTITUDE OF THE MIDDAY SUN > p. 7
The 'Twilight' Trap: While the Sun doesn't set at the Arctic Circle on June 21, the duration of 'Twilight' (time between sunset and complete darkness) increases as you move poleward from the Equator. A future statement might ask: 'The duration of twilight is minimum at the Equator and maximum at the Poles.' (True, due to the steep angle of the sun's path at the Equator).
Use the 'Hemisphere Filter'. 21st June is Northern Summer. Immediately eliminate Option B (Antarctic/South) and Option D (Capricorn/South). You are left with A (Arctic) and C (Equator). Basic logic: The Equator has equal day/night year-round, so 'special' solar events like the Solstice usually refer to the Tropics or Polar circles. Option A is the definition of the Solstice.
Mains GS-1 & GS-3 (Energy): Link the 'Overhead Sun' concept to the International Solar Alliance (ISA). The ISA framework targets countries 'lying fully or partially between the Tropics' specifically because these are the zones that receive direct vertical insolation, maximizing solar photovoltaic efficiency.