7. Draw graticules for azimuthal equidistant projection using the following data: Radius of the earth: 1: 635,000,000 Scale: 1: 200, 000,000 Longitudinal interval: 30⁰ Longitudinal extent: 0° - 360° Radius of parallel 50º N = Radius of parallel 70° N= Latitudinal interval: 10⁰ Latitudinal extent: 30° N - 90° N. Radius of parallel 600 N= Radius of parallel 800 N=​

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Answer 1

The Radius of parallel 80º N based on the information is 105,664,862.

How to explain the information

It should be noted that to draw graticules for azimuthal equidistant projection, we need to first determine the scale factor, which is the ratio of the actual size of the earth to the size on the map.

Scale factor = 1/200,000,000

Next, we need to determine the distance between each latitude and longitude line. For the longitudinal interval of 30⁰, we divide 360⁰ by 30⁰ to get 12 lines.

For the latitudinal interval of 10⁰, we subtract the latitudinal extent of 30° N from 90° N to get 60° of latitude. We then divide 60° by 10⁰ to get 6 lines.

We also need to determine the radius of each parallel. Since the radius of the earth is given as 635,000,000, we can calculate the radius of each parallel using the formula:

Radius of parallel = Radius of earth * cos(latitude)

For latitude 50° N:

Radius of parallel 50º N = 635,000,000 * cos(50°) = 452,242,300

For latitude 70° N:

Radius of parallel 70º N = 635,000,000 * cos(70°) = 222,560,702

For latitude 60° N:

Radius of parallel 60º N = 635,000,000 * cos(60°) = 318,198,051

For latitude 80° N:

Radius of parallel 80º N = 635,000,000 * cos(80°) = 105,664,862

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Related Questions

At what depth range below the earth's surface is the asthenosphere located?

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Answer: The asthenosphere is located approximately 80-200 km below the Earth's surface.

Explanation: The asthenosphere is located in the mantle of the Earth, which lies below the Earth's crust. More specifically, the asthenosphere is located in the upper mantle, at a depth range of approximately 80-200 km (50-120 miles) below the Earth's surface.The mantle itself is also divided into other layers, including the upper mantle, the transition zone, and the lower mantle. The asthenosphere is part of the upper mantle and is characterized by its viscous, plastic-like behavior, which allows for the movement of tectonic plates.Therefore, the asthenosphere is located approximately 80-200 km below the Earth's surface.

Does anyone know the right answers? I got these wrong.

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As temperature increases, water vapor capacity of air increases

As temperature decreases, water vapor capacity of air decreases

As temperature increases, relative humidity decreases if the amount of water vapor in the air remains the same

As temperature decreases, relative humidity increases if the amount of water vapor in the air remains the same.

How to explain the information

As temperature increases, the water vapor capacity of air also increases. This means that warmer air can hold more water vapor than cooler air. Conversely, as temperature decreases, the water vapor capacity of air decreases as well.

Relative humidity, on the other hand, is the amount of water vapor in the air compared to the maximum amount of water vapor that the air can hold at a particular temperature. As the temperature increases, the relative humidity decreases if the amount of water vapor in the air remains the same. This is because the air can hold more water vapor at higher temperatures, so the same amount of water vapor will be a smaller fraction of the maximum water vapor capacity.

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what does the oceans connection to earth's water reservoirs through evaporation and precipitation tell you about the oceans role in the water cycle

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Answer:

The oceans are, by far, the largest storehouse of water on earth — over 96% of all of Earth's water exists in the oceans. Not only do the oceans provide evaporated water to the water cycle, they also allow water to move all around the globe as ocean currents.

Explanation:

The ocean is a huge storehouse of water

When we talk about the water cycle, we must consider both where water is stored in pools, and the fluctuation of water between those storehouses. Much more water is "in storage" for long periods of time than is actively moving through the cycle. It is estimated that of the 332,500,000 cubic miles (mi3) (1,386,000,000 cubic kilometers (km3)) of the world's water supply, about 321,000,000 mi3 (1,338,000,000 km3) is stored in oceans. That is about 96.5 percent of all Earth's water. It is also estimated that the oceans supply about 90 percent of the evaporated water that goes into the water cycle.

The water in the oceans is saline (saltwater). Saline water contains significant amounts (referred to as "concentrations") of dissolved salts. In this case, the concentration is the amount (by weight) of salt in water, as expressed in "parts per million" (ppm). Water is saline if it has a concentration of more than 1,000 ppm of dissolved salts; ocean water contains about 35,000 ppm of salt.

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