Solar Radiation & Earth's Seasons Simulation (1)

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University of Notre Dame *

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Geography

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Jan 9, 2024

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Name:___________________________________________ Date:____________________ Pd:_____ Valery Sepulveda 1st Period Sunrise, Sunset Worksheet Part 1. Motions of the Sun 1. Using your computer, go to the online “Motions of the Sun” simulator found at http://astro.unl.edu/naap/motion3/animations/sunmotions.html 2. Begin by setting the observer’s latitude to your latitude by adjusting the “arrow bar” across the world map on the right. My latitude is:___ _56.4 N_______ _______ 3. Familiarize yourself with the simulator by experimenting with the “time and location controls” and the “animation controls.” 4. Use the controls to manipulate the motions of the sun to answer the questions. 5. Move the hands on the clock to the sunrise and sunset of each date. Then complete the chart below: Date Sunrise Time Sunrise Location (N, S, E, W, NE, SE, NW or SW) Sunset Time Sunset Location (N, S, E, W, NE, SE, NW or SW) Number of daylight hours March 21st 6:05 AM E 6:11 PM W 12 hours June 21st 3:20 AM NE 8:45 PM NW 17-18 Hours September 21st 5:50 AM E 5:55 PM W 12 hours December 21st 8:42 AM SE 3:16 PM SW 6-7 hours A. What do you think is causing the difference in day lengths? The difference in day lengths is caused by the tilt of the Earth's axis. During different times of the year, different parts of the Earth receive varying amounts of sunlight, resulting in longer or shorter days. B. What effect do you think the length of day will have on temperature? The length of the day can have an effect on temperature. Generally, longer days mean more time for the sun to heat up the Earth, so temperatures tend to be warmer. On the other hand, shorter days mean less time for the sun to warm things up, so temperatures can be cooler. Part 2. Seasons and Ecliptic 1. Now go to the online “Seasons and Ecliptic” simulator found at http://astro.unl.edu/naap/motion1/animations/seasons_ecliptic.html . 2. Set the observer’s latitude to your latitude by adjusting the stick figure on the globe on the right. 28.5 N 3. Familiarize yourself with the simulator by experimenting with the controls. 4. Use the controls to manipulate the Earth’s orbit, notice the changes to the incoming sunlight to answer the questions. 5. Change the dates to observe the Sunlight angle (Sun’s altitude) and the sunbeam spread.
Date March 21st June 21st September 21st December 21st Sun’s altitude 61.5 Degrees 84.9 Degrees 60.9 Degrees 38.1 Degrees Draw the angle of the arrows Describe the sunbeam spread The sunbeam spread refers to the angle at which sunlight spreads out or diverges. It is aver age. The sunbeam spread is looking very average and the suns right ascension is 23. Hours. The sunbeam spread is average on Sept. 21. It is wider than the sunbeam on Dec 21. The sunbeam spread looks larger or elongated on Dec. 21. It is very narrow and deep. Draw the sunbeam spread C. How does the sunbeam spread impact the amount of sunlight per area? The sunbeam spread impacts the amount of sunlight per area by determining how concentrated or spread out the sunlight is. A narrower sunbeam spread means the sunlight is more concentrated, providing more intense sunlight per area. A wider sunbeam spread results in less concentrated sunlight, spreading it out over a larger area. So, the sunbeam spread affects the intensity of sunlight received in a given area. D. What effect do you think varying Sun angle and sunbeam spread will have on temperature? Why? The varying sun angle and sunbeam spread can have an impact on temperature. When the sun angle is higher and the sunbeam spread is narrower, the sunlight is more concentrated, leading to higher temperatures. On the other hand, when the sun angle is lower and the sunbeam spread is wider, the sunlight is more spread out, resulting in lower temperatures. So, the angle and spread of the sun's rays play a role in determining temperature. E. On which date does the Northern Hemisphere receive the longest number of daylight hours? How is this related to the angle of the Sun’s altitude and the sunbeam spread? In the Northern Hemisphere, the longest number of daylight hours is typically receive around June 21st, which is the summer solstice. This is related to the angle of the Sun's
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