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It depends on the time of day because the angle of the sun will determine the shadow length
The answer depends on the information that you have. If the arc subtends an angle of x radians in a circle with radius r cm, then the arc length is r*x cm.
The sea would get essentially the same amount of sun as neighboring land of the same latitude. The difference being there aren't significant hills or valleys so it would be more evenly distributed (at the same latitude) Obviously different latitudes would differ with the length of day. Areas within the artic circle will have periods of sunlight 24 hrs a day, and periods of darkness 24 hrs a day.
Earth gets 24 hours of sunlight each day. There is always 50% of the Earth illuminated by the sun.
1) Where at in Florida? Florida is a long state, and that will account for a large difference in the sun angle. 2) What day and time are you talking about? The sun angle varies from season to season, day to day, and minute to minute.
The length of the day and the length of the seasons
its gives it a boner
To collect the most sunlight. The angle relates to the angle the sunlight comes into your area. Aiming it directly at the sun all day would maximize solar collection.
It will Lengthen and shorten during the day, as the angle of the sun changes
During the summer, the sun is striking the Northern Hemisphere straight on, therefore providing strong sunlight and longer daylight hours. The opposite is true during the winter; the Northern Hemisphere is turned away from the sun during this time, hence receiving weak sunlight and shorter daylight hours.
Shadows appear tallest in the morning because the sun is low on the horizon, casting longer shadows due to the angle of sunlight. As the day progresses, the sun rises higher, reducing the length of shadows.
1) The angle at which the sunlight hits the ground (more acute as you approach the poles. 2) The variable length of "day". 3) Terrine, the planet is not smooth.
If you mean the length of the day, yes - that is the same around the Earth. The Earth rotates as a rigid body. If by day length you mean hours of sunlight. On the same lines of latitude day length will be the same, but due to the wobble in the rotation of the earth, day length is different along lines of longitude.
Because of the amount of sunlight changing from the earth being on its axis
Some plants need more sunlight then others to reproduce and some need less.
That depends upon the time of day, which day of the year it is and where the person is. The shadow length depends upon the angle of the sun above the horizon: shadow_length = height_of_person ÷ TAN(angle_of_sun_above_horizon)
With no atmosphere, there would be no "twilight". Twilight is caused by the scattering of sunlight in the atmosphere. With no atmosphere, you'd go from "day" to "night" with nothing in between.