10 metres

12 miles per hour

Wind shear is quantified as the exponent α (alpha) in the power law equation that relates wind speeds at two different heights….Power Law

1. V1 = Velocity at height Z.
2. V2 = Velocity at height Z.
3. Z1 = Height 1 (lower height)
4. Z2 = Height 2 (upper height)
5. α = wind shear exponent.

Going up in altitude, the pressure gradient between the warm air and the cold air increases with height. slow the air as it collides into them. The influence of this friction is less with height above the ground, thus the wind speed increases with height.

The name for wind blowing with very high speed at height of 3 kilometre from the upper atmosphere is called jet stream. The upper atmosphere is called Exosphere. Its range lie from sea level is 700 km to 10,000 km above the earth surface.

The winds, whether generated by a coastal storm or an afternoon summer sea breeze, blow faster over the ocean than over the land because there is not as much friction over the water. The oceans do not have these impediments, which impart friction, therefore; the wind can blow at a greater velocity.

As altitude rises, air pressure drops. In other words, if the indicated altitude is high, the air pressure is low. As altitude increases, the amount of gas molecules in the air decreases—the air becomes less dense than air nearer to sea level.

The depth (distance from top to bottom) of the atmosphere is greatest at sea level and decreases at higher altitudes. With greater depth of the atmosphere, more air is pressing down from above. Therefore, air pressure is greatest at sea level and falls with increasing altitude.

Russia

Standard atmospheric pressure is usually taken to be 0.760mHg at 0°C. This is a pressure of 101325 Pa. In this text when solving problems we shall assume P0=105Pa.

Answer. Air pressure is greater at sea level than at the top of a mountain. The amount of air at sea level is greater than that on top of a mountain.

Answer: Less depth means less pressure. At the top of Mount Everest, Earth’s highest mountain, air pressure is one-third of what it is at sea level.

Pressure at the top of a mountain… Atmospheric pressure reduces with altitude for two reasons, both of which are related to gravity. Molecules further away from the earth have less weight (because gravitational attraction is less) but they are also ‘standing’ on the molecules below them, causing compression.

Air pressure is higher at lower altitudes. Air density is higher at lower altitudes. There is more space between air molecules at higher altitudes. There is less oxygen to breathe at the top of a high mountain than there is at sea level.

Air pollution is affected by change in altitude. Consequently, mobile sources designed to operate at pressures of one atmosphere perform less efficiently at high altitudes and emit greater amounts of hydrocarbons and carbon monoxide than those designed to operate at the lower atmospheric pressures.

Air pressure is greater at the bottom of a mountain as the air is more dense there. There are more Elements in air where it is dense thus more pressure as it is the force exerted per unit area so if there are more Particles, more force will be exerted on any surface.

But why should the top of a mountain be colder than the bottom? At the top of a mountain, air cools because as air rises it cools. If the air pressure is 1000 millibar, that is because there is approximately 10 tonnes of air above every square metre of ground. This air pressure is literally pressing down on everything.

As you increase in elevation, there is less air above you thus the pressure decreases. As the pressure decreases, air molecules spread out further (i.e. air expands) and the temperature decreases.

Because the earth’s axis is tilted. It is all about the tilt of the Earth’s axis. Many people believe that the temperature changes because the Earth is closer to the sun in summer and farther from the sun in winter. In fact, the Earth is farthest from the sun in July and is closest to the sun in January!

When we heat air, the molecules jiggle and zip around faster, which causes them to spread out. When a mass of air takes up more space, it has a lower density. Warm air rises when it’s surrounded by cold air because of its lower density. Yes, that’s due to heat, but density is the main factor causing the movement here.

The sun is a bolus of gas and fire measuring around 27 million degrees Fahrenheit at its core and 10,000 degrees at its surface. Meanwhile, the cosmic background temperature—the temperature of space once you get far enough away to escape Earth’s balmy atmosphere—hovers at -455 F. How can this be?

You’d think that the Sun’s surface would be hotter than its outer atmosphere, since, the surface is closer to the nuclear furnace at the Sun’s core. But the further you get from the sun’s surface, the hotter the atmosphere seems to get.

Since the temperature of the Earth is so much hotter than space, you’d expect that the closer you get to space the colder it gets. So the air is densest closest to the surface of the Earth, then it gradually becomes less dense until you get to the vacuum of space.

2 Answers. If the Earth was a mile closer, temperature would increase by 5.37×10−7% . For the change in temperature to be noticeable, Earth would have to be 0.7175% closer to the sun.

Because the equator is closer to the sun. Because the sun’s rays hit the earth’s surface at a higher angle at the equator.

The countries through which the equator runs are:

• São Tomé and Principe.
• Gabon.
• Republic of the Congo.
• The Democratic Republic of the Congo.
• Uganda.
• Kenya.
• Somalia.
• Maldives.

If you live on the equator you will experience the quickest rates of sunrise and sunset in the world, taking a matter of minutes. While tropical areas along the equator can experience wet and dry seasons, other regions may well be wet for much of the year.