conclusion of tropical cyclone

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Answer 1

Answer:

Explanation:

In conclusion, tropical cyclones are powerful and dangerous weather events that can cause extensive damage to coastal regions. These storms are characterized by their strong winds, heavy rainfall, storm surge, and potential for tornadoes. It is important for individuals living in hurricane-prone areas to stay informed about storm developments and to take appropriate precautions to protect themselves and their property. Governments and emergency response organizations should also have disaster plans in place to ensure effective responses to tropical cyclones. With careful planning and preparation, communities can minimize the impact of these devastating storms and work towards rebuilding and recovery in their aftermath.

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Related Questions

. Draw a graticules for Cylindrical Equal-Area Projection for the whole globe on the scale= 450,000,000 spacing the parallels at 15° and the meridians at 30°. Calculate the projections a) Change the radius of the globe (the earth) using the scale b) Determine the length of the equator on the globe. c) Determine the number of interception points of the meridians along the equator/ parallel.d) Along the equator mark off the correct meridian distances e) Based on the distance indicated above, make divisions on the equator and draw in the meridians as straight lines through these points. f) To decide the interception points of the parallels along the meridians.

Answers

The Cylindrical equal-area projection is a map composition that utilizes an erected cylinder to denote the entirety of the globe, ensuring the plateau area for each region is uniformly maintained.

What is the projection about?

While executing this process does not alter overall sizes of various regions, north and south extremities of the cylinder do bare disparities in angles, and thus shapes are distorted around these poles.

Graticules describes the lines etched upon the exterior of a mapped paper. Made up of parallels (lines of latitude) and meridians (longitude), their evenly spaced intervals vary according to the projection's scale as well as radius--increasing the world's circumference will consequently reduce its size.

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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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Determine the measure of each angle in the triangle shown below:

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The measures of the angles in the triangle are:

X ≈ 48.6°; W = 41.4°

How to Determine the Measure of each Angle in the Triangle?

The triangle is a right triangle, so we will apply the Trigonometric ratios to solve for for one of the angles in the image given.

To find angle X, apply the sine ratio (SOH):

sin ∅ = opp/hyp

sin X = 6/8

X = sin^(-1)(6/8)

X ≈ 48.6°

All angles in a triangle is equal to 180 degrees when added together, therefore:

angle W = 180 - 90 - 48.6

measure of angle W = 41.4°

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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=​

Answers

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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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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An ocean current is a constant flow of water along a path in the ocean. If the current is close to the surface, it is called a surface current. Ocean currents can have a great effect on the planet, influencing weather patterns and affecting wildlife. Today, you are going to get the chance to map out these surface currents and analyze your results. Read all of the directions carefully before you begin.

Directions
Draw the ocean surface currents on this map using digital or physical drawing tools.
Locate the following on your worksheet.
Two major surface currents in the Atlantic Ocean (one in each hemisphere)
Two major surface currents in the Pacific Ocean (one in each hemisphere)
One major surface current in the Indian Ocean
Draw and label each of these major currents according to the following guidelines:
A directional arrow must show the direction of the flow of each current.
Label each current with the correct name.
Cold currents must be represented by blue arrows and blue-text labeling.
Warm currents must be represented by red arrows and red-text labeling.
Once you have diagrammed the surface currents, answer each of the conclusion questions.

Answers

The Gulf Stream and the North Atlantic Drift are the two main surface currents in the Atlantic Ocean.The California Current and the Kuroshio Current are the two main surface currents in the Pacific Ocean.The Agulhas Current is the main surface current in the Indian Ocean.What is Atlantic Ocean?

With a surface area of over 106,400,000 square kilometres, the Atlantic Ocean is the second-largest ocean in the world. About 20% of the Earth's surface is covered by it, and 29% of the ocean surface area. The North Atlantic Ocean and the South Atlantic Ocean are the two sections of the Atlantic Ocean.

It is bordered by the Southern Ocean to the east and south, the Indian Ocean to the south, the Pacific Ocean to the west, and the Arctic Ocean to the north. The Caribbean Sea, the Gulf of Mexico, and the Mediterranean Sea link the Atlantic Ocean to the other oceans. Diverse marine species, including as sharks, whales, seals, dolphins, and tuna, call it home.

In the Atlantic Ocean, the Gulf Stream and the North Atlantic Drift are the two main surface currents.In the Pacific Ocean, the California Current and the Kuroshio Current are the two main surface currents.In the Indian Ocean, the Agulhas Current is a significant surface current.

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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.

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