Consider the following statement:1. The mid-day sun never shines overh...
Statement 1 is correct. The Tropic of Cancer and the Tropic of Capricorn mark the furthest points north and south, respectively, where the sun can be directly overhead. Beyond these latitudes, the mid-day sun will never shine directly overhead.
Statement 2 is incorrect. The angle of the sun's rays actually decreases towards the poles, not increases. This is because the Earth's curvature causes the sun's rays to be more spread out at higher latitudes.
Therefore, the correct answer is 3) 1 only.
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Consider the following statement:1. The mid-day sun never shines overh...
Above the horizon is always less than 90 degrees at any location on Earth, except at the North and South Poles where it can be exactly 90 degrees during the summer solstice.
These statements are both true. The Tropic of Cancer and the Tropic of Capricorn are two latitudes located at approximately 23.5 degrees North and South of the equator, respectively. The sun appears directly overhead at noon on the day of the summer solstice (around June 21st) at the Tropic of Cancer, marking the beginning of summer in the Northern Hemisphere. Similarly, on the day of the winter solstice (around December 21st), the sun appears directly overhead at noon at the Tropic of Capricorn, marking the beginning of summer in the Southern Hemisphere.
At any other latitude, the angle of the sun above the horizon varies throughout the day and throughout the year, depending on the time of day, the season, and the latitude. This angle is always less than 90 degrees, except at the North and South Poles during the summer solstice, when the sun can be exactly 90 degrees above the horizon (since the poles are located at the Earth's axis of rotation).
Consider the following statement:1. The mid-day sun never shines overh...
Statement 1 is correct .The mid-day sun never shines overhead on any latitude beyond the Tropic of Cancer and the Tropic of Capricorn.
Statement 2 is wrong .The angle of the sun’s rays goes on decreasing towards the poles.
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