Showing posts with label Water vapor. Show all posts
Showing posts with label Water vapor. Show all posts

Sunday, February 14, 2021

WHY DO PLANES LEAVE WHITE TRAILS IN THE SKY? - With so many commercial jets flying routes all over the world, there probably isn’t a person on Earth who hasn’t noticed the white smoke coming from airliners. When flying at high altitudes, jet engines exhaust extremely hot air and water vapor, among other things. The cold temperatures and low pressures at these altitudes result in the water forming into visible ice crystals. The results are white clouds known as contrails, which is short for condensation trails. There are three components necessary for clouds to form in the atmosphere. There must be moisture present in the form of water vapor. The atmosphere must cool enough for that water vapor to condense into visible moisture (either as water droplets or ice crystals). There must be some form of condensation nuclei. The nuclei can be any bit of particulate in the atmosphere, like dust or pollution, that water molecules can hold onto. Most clouds you see are the result of moist warm air rising. As it gets higher, the air cools down to the temperature of the surrounding air. When it reaches the dew point, a visible cloud forms. Condensation trails behind aircraft are simply clouds. All three components are created, and when conditions are just right, these contrails will appear behind every plane in that part of the sky. Jet engines produce an incredible amount of heat, along with water vapor and other combustion exhaust particles like carbon dioxide.

An airliner leaves contrails as it passes the Moon
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Why do Planes Leave White Trails in the Sky?

BY MATT CLAIBORNE

 

 

With so many commercial jets flying routes all over the world, there probably isn’t a person on Earth who hasn’t noticed the white smoke coming from airliners.

But why do these streaks only occur behind some planes?

Are they dumping fuel?

Is it hazardous?

What exactly are these vapor trails?

Why Planes Leave Trails

When flying at high altitudes, jet engines exhaust extremely hot air and water vapor, among other things.

The cold temperatures and low pressures at these altitudes result in the water forming into visible ice crystals.

The results are white clouds known as contrails, which is short for condensation trails.

The Science Behind Contrails

There are three components necessary for clouds to form in the atmosphere.

There must be moisture present in the form of water vapor.

The atmosphere must cool enough for that water vapor to condense into visible moisture (either as water droplets or ice crystals).

There must be some form of condensation nuclei. The nuclei can be any bit of particulate in the atmosphere, like dust or pollution, that water molecules can hold onto.

Most clouds you see are the result of moist warm air rising.

As it gets higher, the air cools down to the temperature of the surrounding air. When it reaches the dew point, a visible cloud forms.

Condensation trails behind aircraft are simply clouds. All three components are created, and when conditions are just right, these contrails will appear behind every plane in that part of the sky.

Jet engines produce an incredible amount of heat, along with water vapor and other combustion exhaust particles like carbon dioxide. This exhaust is shot out the back of the jet engine into the surrounding cold air.

The atmosphere at high altitudes is frigid. Most airliners fly between 30,000 and 38,000 feet above sea level, where the temperatures range between -45 and -61 degrees Celsius.

At these temperatures, the water vapor will condense into water droplets, which will become ice crystals quickly.

Like the upper-level cirrus clouds at these altitudes, the ice crystals will blow and scatter with the wind conditions. If the upper-level winds are calm, the contrails may remain intact for a long time.

While it is true that the contrails contain pollutants, just as all combustion engines leave pollutants when operating, the contrails are not made of smoke, visible pollution, or chemicals.

They are clouds just like natural cirrus clouds, made of ice crystals suspended in the atmosphere.

Why Don’t All Planes Leave White Smoke?

A specific set of atmospheric circumstances have to line up to create an exhaust contrail.

It’s seldom cold enough at lower altitudes for this to happen, so the primary place they occur happens to be at the cruising altitude of jets.

You aren’t likely to see contrails behind propeller-driven aircraft or low-flying planes. It’s also why the presence of contrails varies from day to day, depending on the weather conditions present in the upper atmosphere.

Classifications of Exhaust Contrails

NASA’s Langley Research Center has studied contrails and their effects for decades. They divide contrails up based on how persistent they are in the atmosphere.

Contrails are ranked as short-lived, persistent, and persistent-spreading.

Aerodynamic Contrails

The process described above is known as an exhaust contrail since it is formed behind the engines. But the wings and control surfaces can cause a similar phenomenon, known as aerodynamic contrails.

Persistent spreading contrails

Aerodynamic contrails are more likely to be visible near the surface in areas with a lot of moisture already in the atmosphere.

When riding in a plane and looking out the window, you may see clouds form on top of the wing or in the vortices trailing behind it. They tend to happen quickly as the plane travels between different levels in the atmosphere.

As the air over the top of the wing accelerates, it also cools. If there’s enough water vapor in the atmosphere and the temperatures are close to the dew point, this cooling is enough to create a cloud.

These clouds take several forms, depending on how the aircraft is configured.

F/A-18 Hornet in flight with aerodynamic contrails
over the wings and in the wingtip vortices.


In some cases, a smooth cloud forms perfectly over the wings of the plane. In other cases, the accelerated air flowing behind the air in the wingtip vortices creates a cloud. 

Since the cloud shows the area of lower pressure over the wing, it changes as the pilot controls the lift made by that wing.

As the pilot changes the wing’s angle of attack, the aerodynamic contrails may grow larger or dissipate.

These contrails are especially neat to see since they visually show where the lift is being generated and where the wake turbulence lies. It’s a physical and visual manifestation of something you usually only learn about theoretically.

Any aircraft can leave aerodynamic contrails. They can form at any altitude as long as the atmospheric conditions are just right. They’re even often seen on the nose cones of rockets on liftoff!

Conspiracy Theories

Aviation, by its very nature, is a technical subject that involves a lot of science and technical jargon. Sometimes, when the non-flying public is unaware of the science behind it, conspiracy theories can pop up.

Why Do Planes Dump Fuel?

Some people believe that the white trails behind aircraft are fuel because they’ve heard of pilots “dumping fuel” in the movies.

Some aircraft are indeed equipped to be able to dump their jet fuel overboard. This is an emergency procedure designed to reduce the landing weight of an airplane.

Transport aircraft are often designed to take off at much higher weights than they can land. Since under normal conditions, the plane will burn thousands of pounds of fuel between its departure and destination, the plane will be well within limits before landing.

But what about in the case of an emergency, can the plane land safely if something goes wrong right after takeoff?

In some cases, the answer is no. The fuel needs to be burned off by remaining in the air or dumped overboard to enable the plane to land immediately.

Dumping of fuel is extremely rare and carefully controlled. It would only happen over unpopulated areas, and remaining aloft until a safe landing can be accomplished is always the preferable solution.

The vapor trails left by a plane at altitude have nothing to do with dumping fuel.

 “Chemtrails”

Another popular conspiracy theory is that aircraft are being used by the world’s governments to disperse chemicals into the atmosphere.

This theory has resulted in the term “chemtrails,” which is becoming more and more common.

Some believe they are related to a secret government atmospheric control program involving cloud seeding and weather manipulation.

Effects of Contrails on Climate

One area of valid research and study has been done on whether or not the presence of contrails in the atmosphere affects the climate.

Several hypotheses have been floated that the contrails, by increasing the amount and coverage of upper-level clouds, reduce sunlight penetration to the surface.

Theoretically, this could reduce surface temperatures. But they also trap in heat, so research needed to be done to find out whether the clouds have a net warming or cooling effect.

NASA has studied the effects carefully, and the results show a minor net warming effect.

Observationally, they’ve shown that warming is more pronounced in areas with the most flight activity, like over the North Atlantic flight corridor between America and Europe.

Matt Claiborne

Airline Transport Pilot. Certified Flight Instructor-Airplane, Single and Multiengine Instrument

https://www.aircraftcompare.com/blog/why-planes-leave-white-trails/


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Chemtrails Versus Contrails

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Why planes dump fuel

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https://puricare.blogspot.com/2020/08/why-planes-dump-fuel-pilot-will-choose.html

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Chemtrails And Cnspiracy Theories

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https://puricarechronicles.blogspot.com/2017/12/chemtrails-and-conspiracy-theories-jet.html

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Butterfly Wings

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Going Nowhere… Successfully

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A Lesson From the “Miracle on the Hudson”

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https://puricarechronicles.blogspot.com/2019/12/a-lesson-from-miracle-on-hudson-that.html


Monday, January 18, 2021

PRECIPITATION - Precipitation is needed to replenish water to the earth. Without precipitation, this planet would be an enormous desert. The amount and duration of precipitation events affect both water level and water quality within an estuary. Precipitation supplies freshwater to estuaries, which is an important source of dissolved oxygen and nutrients.- Precipitation is any form of water that falls to the earth’s surface. This includes snow, rain, sleet, freezing rain, and hail. Precipitation is generated in clouds. When water vapor droplets in clouds become so large that updrafts within the clouds can no longer support them, the water will fall to the earth under the force of gravity. Why is Precipitation Important? Precipitation is needed to replenish water to the earth. Without precipitation, this planet would be an enormous desert. The amount and duration of precipitation events affect both water level and water quality within an estuary. Precipitation supplies freshwater to estuaries, which is an important source of dissolved oxygen and nutrients. Droughts lower the freshwater input to estuaries and the water levels of inland lakes. Lake levels influence water drainage and circulation patterns in freshwater estuaries. How is Precipitation measured? Precipitation is typically reported in millimeters or inches of liquid precipitation. This amount is typically added over a certain period of time, such as inches per day.

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Precipitation

Precipitation is needed to replenish water to the earth. Without precipitation, this planet would be an enormous desert. 

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The amount and duration of precipitation events affect both water level and water quality within an estuary. Precipitation supplies freshwater to estuaries, which is an important source of dissolved oxygen and nutrients.

By Fondriest Staff 


 

Precipitation is any form of water that falls to the earth’s surface. This includes snow, rain, sleet, freezing rain, and hail.

Precipitation is generated in clouds.

When water vapor droplets in clouds become so large that updrafts within the clouds can no longer support them, the water will fall to the earth under the force of gravity.

Why is Precipitation Important?

Precipitation is needed to replenish water to the earth.

Without precipitation, this planet would be an enormous desert.

The amount and duration of precipitation events affect both water level and water quality within an estuary.

Precipitation supplies freshwater to estuaries, which is an important source of dissolved oxygen and nutrients.

Droughts lower the freshwater input to estuaries and the water levels of inland lakes.

Lake levels influence water drainage and circulation patterns in freshwater estuaries.

How is Precipitation measured?

Precipitation is typically reported in millimeters or inches of liquid precipitation.

This amount is typically added over a certain period of time, such as inches per day.

Precipitation Technology

Precipitation can be measured in a numerous ways.

One precipitation measuring instrument is known as a “tipping-bucket rain gauge.”

A tipping bucket rain gauge uses a small cup that fills with precipitation.

When the cup is full, it will tip and empty.

A counter tracks how many times the cup tips, and after a certain time interval, this number is converted to a precipitation measurement in millimeters.

Heated tipping bucket rain gauges allow the measurement of snow and sleet.

Located in the Lower Great Lakes and Ohio River Valley region, Fondriest Environmental is a leading distributor and integrator of equipment for natural resource professionals and outdoor enthusiasts. Our team of specialists can help customers understand the products they are buying and make the correct decisions out in the field. We seek to understand project needs, devise a comprehensive solution, provide the equipment and know-how to implement it, and then offer long-term project support for whatever needs arise.

https://www.fondriest.com/news/precipitation.htm


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Severe Weather And Clouds

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Rain Clouds

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Chance of Rain

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Water Cycle

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Flawless Design of Water Makes Life Possible

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All the Fountains of the Deep

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Ask for rain. Ask for more rain

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Thursday, December 24, 2020

WHAT IS HUMIDITY? - How is it measured?- Easily stated humidity is simply the amount of water vapor held in the air. Water vapor is the gaseous state of water. As the temperature of the air increases more water vapor can be held since the movement of molecules at higher temperatures prevents condensation from occurring. There are three main measurements of humidity: relative, absolute and specific. Absolute humidity (units are grams of water vapor per cubic meter volume of air) is a measure of the actual amount of water vapor in the air, regardless of the air's temperature. The higher the amount of water vapor, the higher the absolute humidity. For example, a maximum of about 30 grams of water vapor can exist in a cubic meter volume of air with a temperature in the middle 80s. Relative humidity, expressed as a percent, is a measure of the amount of water vapor that air is holding compared the amount it can hold at a specific temperature. Warm air can possess more water vapor (moisture) than cold air, so with the same amount of absolute/specific humidity, air will have a higher relative humidity. A relative humidity of 50% means the air holds on that day (specific temperature) holds 50% of water needed for the air to be saturated. Saturated air has a relative humidity of 100%. The relative humidity of an air-water mixture is also defined as the ratio of the partial pressure of water vapor in the mixture to the saturated vapor pressure of water at a given temperature (See what is vapor pressure). Thus the relative humidity of air is a function of both water content and temperature. Specific humidity refers to the weight of water vapor contained in a unit weight of air.

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Sper Scientific Sling Psychrometer to Measure Humidity 
 Top is wet bulb -- Bottom is dry bulb

What is  humidity?

How is it measured?

edinformatics.com


 

What is Humidity?

Easily stated humidity is simply the amount of water vapor held in the air.

Water vapor is the gaseous state of water.

As the temperature of the air increases more water vapor can be held since the movement of molecules at higher temperatures prevents condensation from occurring.

There are three main measurements of humidity: relative, absolute and specific.

Absolute humidity (units are grams of water vapor per cubic meter volume of air) is a measure of the actual amount of water vapor in the air, regardless of the air's temperature.

The higher the amount of water vapor, the higher the absolute humidity.

For example, a maximum of about 30 grams of water vapor can exist in a cubic meter volume of air with a temperature in the middle 80s.

Relative humidity, expressed as a percent, is a measure of the amount of water vapor that air is holding compared the amount it can hold at a specific temperature.

Warm air can possess more water vapor (moisture) than cold air, so with the same amount of absolute/specific humidity, air will have a higher relative humidity.

A relative humidity of 50% means the air holds on that day (specific temperature) holds 50% of water needed for the air to be saturated.

Saturated air has a relative humidity of 100%.

The relative humidity of an air-water mixture is also defined as the ratio of the partial pressure of water vapor in the mixture to the saturated vapor pressure of water at a given temperature (See what is vapor pressure).

Thus the relative humidity of air is a function of both water content and temperature.

Specific humidity refers to the weight of water vapor contained in a unit weight (amount) of air (expressed as grams of water vapor per kilogram of air).

Absolute and specific humidity are quite similar in concept.

What is Dew Point?

Dew Point is the temperature at which air is saturated with water and condensation begins. The higher the dew point rises, the greater the amount of moisture in the air.

What is the relationship between Dew Point and Relative Humidity?

Compared to relative humidity, dew point is frequently cited as a more accurate way of measuring the humidity and comfort of the air, since it is an absolute measurement (unlike relative humidity).

The relative humidity is 100 percent when the dew point and the temperature are the same.

If the temperature drops any further, condensation will result, and liquid water will begin to form.

If the relative humidity is 100 percent (i.e., dew point temperature and actual air temperature are the same), this does not necessarily mean that precipitation will occur.

It simply means that the maximum amount of moisture is in the air at the particular temperature the air is at.

Saturation may result in fog on the ground and clouds aloft (which consist of tiny water droplets suspended in the air).

While dew point gives one a quick idea of moisture content in the air, relative humidity does not since the humidity is relative to the air temperature.

In other words, relative humidity cannot be determined from knowing the dew point alone, the actual air temperature must also be known.

Relative humidity is also approximately the ratio of the actual to the saturation vapor pressure.

RH = (Actual Vapor Pressure) / (Saturation Vapor Pressure) X 100%

Where actual vapor pressure is a measurement of the amount of water vapor in a volume of air, and increases as the amount of water vapor increases.

Saturated vapor pressure is the maximum VP that can exist at any given temperature.

Air which is at 100% relative humidity (RH) contains water vapor whose VP is its SVP at the given temperature. This corresponds to air which is in equilibrium with liquid water.

RH is the ratio VP/SVP expressed as a percentage. 'Dry' air will contain water vapor with a VP which is less than the SVP at the given temperature.

How is humidity measured?

A device to measure relative humidity is called a hygrometer.

The simplest hygrometer - a sling psychrometer - consists of two thermometers mounted together with a handle attached on a chain.

One thermometer is ordinary. The other has a cloth wick over its bulb and is called a wet-bulb thermometer.

How does a psychrometer measure relative humidity?

A psychrometer also called a sling psychrometer has two thermometers attached.

One is dry (often called the dry bulb thermometer) and measures the actual air temperature.

The other called the wet bulb thermometer has a wet cloth at the tip.

As water molecules evaporate from the surface of the wet bulb they will take heat with them lowering the reading on the thermometer.

The rate of evaporation depends on the vapor pressure or amount of water vapor in the air.

At 100% relative humidity no water will evaporate from the wet bulb and the readings on both thermometers will be the same.

Comparing the two temperatures in a chart will give the relative humidity.

ABOUT THE EDINFORMATICS SCIENCE CHALLENGE

Intermediate school is designed to provide a strong foundation for students in science in order to prepare them for the high school science sequence consisting of biology, chemistry and physics. Although there is some controversy that students are being over-tested on a yearly basis, an eighth grade science test should remain a cornerstone in science assessment.

https://www.edinformatics.com/math_science/what-is-humidity.html


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