The stratosphere is the second major layer of the Earth's atmosphere, located between the troposphere and the mesosphere. It contains the ozone layer, which absorbs up to 99% of ultraviolet radiation from the Sun. Commercial aircraft, such as jet airliners, typically reach their cruising altitude in the lower levels of the stratosphere, between 30,000 and 42,000 feet. This altitude offers several advantages, including reduced fuel consumption due to lower air density and temperature, smoother flights with less turbulence, and faster travel times due to decreased air resistance.
What You'll Learn
- Jet aircraft fly in the stratosphere to reduce turbulence
- Lower air resistance in the stratosphere improves fuel efficiency
- Jet aircraft avoid thunderstorms in the stratosphere
- Jet streams in the stratosphere increase ground speed
- The stratosphere is the highest layer of the atmosphere that aircraft can fly in
Jet aircraft fly in the stratosphere to reduce turbulence
Jet aircraft typically fly in the stratosphere, the second major layer of the Earth's atmosphere, to reduce turbulence and benefit from smoother flights. The stratosphere is very dry, with little water vapour, so there are fewer clouds in this layer than in the troposphere below, where most weather occurs.
The practical reasons for flying in the stratosphere are clear: less turbulence, better fuel economy, and faster flying speeds. Turbulence is often the result of bad weather, which is more common in the troposphere. By flying in the stratosphere, pilots can avoid areas of high turbulence and provide a more comfortable journey for passengers.
In addition, the thin air in the stratosphere means less air resistance, resulting in better fuel efficiency. The air resistance in this layer is about half of that on the ground, allowing planes to maintain airspeed with lower power settings and less fuel. This saves airlines money and contributes to a more efficiently run engine.
Faster flying speeds are also advantageous, especially for commercial flights, as it helps to ensure that flights take off and land on time, meeting passenger expectations. The reduced air friction in the stratosphere increases the true airspeed of the plane, resulting in higher flying speeds.
However, not all aircraft fly in the stratosphere. Some military and commercial aircraft fly in the troposphere, the layer below the stratosphere, where there is low resistance and good lift capacity, resulting in a smoother flight.
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Lower air resistance in the stratosphere improves fuel efficiency
The stratosphere is the second major layer of the Earth's atmosphere, located above the troposphere and below the mesosphere. Commercial airliners typically cruise at altitudes of 9–12 km (30,000–39,000 ft) which is in the lower reaches of the stratosphere in temperate latitudes.
Flying in the stratosphere offers several benefits that improve fuel efficiency. Firstly, the air resistance in the stratosphere is about half of that on the ground, allowing planes to maintain airspeed at lower power settings and, consequently, use less fuel. This is because, in the stratosphere, there is less air density and lower temperatures. The air temperature drops by 2°C or 35.6°F for every 1,000 feet an airplane climbs, up to about 36,000 feet. This results in significant fuel savings for airlines.
Additionally, flying at higher altitudes means less air enters the engine, which further reduces fuel consumption. The more constant the jet-to-fuel ratio is, the better the fuel economy, making stratosphere flying highly advantageous for airlines. By flying in the stratosphere, airlines can also save costs by running their engines more efficiently in the long run.
Furthermore, the thinner air in the stratosphere allows planes to fly faster, increasing their true airspeed (TAS). This is beneficial for commercial flights as it helps them stick to strict schedules and avoid delays. Therefore, the lower air resistance in the stratosphere significantly improves fuel efficiency for commercial airlines.
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Jet aircraft avoid thunderstorms in the stratosphere
The stratosphere is the second major layer of the Earth's atmosphere, sitting just above the troposphere and below the mesosphere. It begins at around 10km (6.2 miles or about 33,000 feet) above the ground and ends at an altitude of 50km (31 miles).
Commercial aircraft, as well as private jets, prefer to fly in the stratosphere due to the benefits of flying at such altitudes. At around 35,000-42,000 feet, the altitude that commercial airliners operate in, a very low amount of oxygen is required for proper combustion in jet engines. This means that planes use less fuel at these altitudes thanks to the lower air density and temperature.
As the troposphere is where most weather phenomena occur, including thunderstorms, planes will fly in the stratosphere to avoid bad weather and turbulence. However, in the case of a very powerful thunderstorm, turbulence can be experienced in the stratosphere. In these instances, pilots will usually navigate around the storm.
The stratosphere is very dry, containing little water vapour, so clouds are unable to form. This means that visibility can be very good. However, there are exceptions. Polar stratospheric clouds (PSC) can be found near the poles in winter in the lower stratosphere.
At higher altitudes, the air is thinner, resulting in less drag. This means that planes can fly faster, an important factor for commercial flights that must adhere to strict schedules.
In summary, jet aircraft avoid thunderstorms in the stratosphere by flying at altitudes where thunderstorms do not occur. They can also navigate around storms if necessary.
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Jet streams in the stratosphere increase ground speed
Jet streams are fast-flowing, narrow, meandering air currents in the Earth's atmosphere. They are the product of atmospheric heating by solar radiation and the Coriolis force, caused by the planet's rotation on its axis. These forces create large-scale circulation cells, which drive the formation of jet streams.
The main jet streams are located near the altitude of the tropopause and are predominantly westerly winds, flowing from west to east. The northern hemisphere has three types of jet streams: the polar jet, the subtropical jet, and the low-level jet. The polar jet flows over the middle to northern latitudes of North America, Europe, and Asia, while the subtropical jet is found at higher altitudes. The northern hemisphere polar jet is the most important for aviation and weather forecasting due to its strength, low altitude, and coverage of many countries.
Jet streams can significantly impact the ground speed of aircraft. By flying with the jet stream, aircraft can increase their ground speed and reduce flight time. For example, flying from Tokyo to Honolulu with the jet stream reduced the trip time by over one-third, from 18 to 11.5 hours. Similarly, flying east across North America can be made faster by about 30 minutes by flying with the jet stream, while flying west against it can increase the time by the same amount.
Additionally, jet streams can provide fuel savings for airlines. As jet streams are located in higher altitudes, where the air density is lower, aircraft engines experience less air resistance, resulting in better fuel efficiency. This is advantageous for airlines as it reduces fuel costs and improves engine efficiency.
However, it is important to note that encountering a jet stream while flying west can reduce ground speed and increase fuel burn, potentially requiring an unscheduled refueling stop. Therefore, flight planning considers jet stream locations to optimize fuel efficiency and avoid unexpected headwinds.
Overall, jet streams in the stratosphere can increase ground speed, reduce flight times, and improve fuel efficiency for aircraft, making them an essential consideration in aviation and flight planning.
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The stratosphere is the highest layer of the atmosphere that aircraft can fly in
The stratosphere is the second major layer of the Earth's atmosphere, located between the troposphere and the mesosphere. It is in this layer that most aircraft reach their cruising altitude.
The stratosphere is where aircraft can fly at optimal fuel efficiency. This is because the air density is lower, meaning less air enters the engine and therefore less fuel is required to fly the plane. This also means that the plane can hold airspeed at lower power settings, resulting in better fuel efficiency. As a general rule, the higher the altitude, the better the fuel economy.
The stratosphere is also where aircraft can fly faster. This is because there is less air friction and an increase in true airspeed (TAS). This is particularly beneficial for commercial flights, as it helps them stick to their strict schedules and avoid delays.
The stratosphere is also the perfect layer to fly in because it experiences the least amount of turbulence. This is because it is very dry, so there are fewer clouds. This makes for a smoother ride overall.
However, it is worth noting that not all aircraft fly in the stratosphere. Some military aircraft, for example, fly in the troposphere, which is the layer below the stratosphere. This is because there is low resistance and good lift capacity in the troposphere, resulting in a smoother flight overall.
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Frequently asked questions
Yes, jet airlines do travel in the stratosphere.
Jet airlines travel in the stratosphere because it is the optimal altitude for fuel efficiency. The air in the stratosphere is thinner, which means less drag and more speed.
The stratosphere is the second major layer of the Earth's atmosphere. It is located below the mesosphere and just above the troposphere.
The stratosphere extends from about 12 to 50 kilometres above sea level.
The temperature in the stratosphere is stratified, with cooler layers closer to the Earth and warmer layers above. The temperature inversion between the stratosphere and the troposphere is most prevalent at their border.