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Optical Phenomena

UK MET office fails to acknowledge particulate aerosol responsible for cloud nucleation

by qbit on Apr.19, 2010, under In the News, Optical Phenomena, What are they?

I’m reposting this propaganda for one reason.  Occasionally I see WW2-era pictures of propeller planes forming thick contrails; even what appear to be persistent chemtrails.   The obvious question to ask is ‘If chemtrails are formed by a jet fuel additive, how do you explain these pictures of thick contrails in old photos of propeller planes?’

The answer is simple.  Lead.  These old propeller planes used lead (tetra ethyl lead) in the fuel as an anti-knock agent.  It doesn’t particularly matter (no pun intended) which metallic aerosol is present in the exhaust.  The nucleation sites still increase water droplet and ice crystal formation and reduce their tendency to evaporate/sublimate into invisible gas in dry high altitude air.  Of course water vapor is a major byproduct of hydrocarbon combustion so if there are nucleation sites present, the water will tend to condense and persist in visible droplets or ice crystals more than if the fuel were clean burning with fewer nucleation sites.

Climate pimps like the UK Met will rarely acknowledge metallic aerosols  when discussing persistent contrail formation.  They will only refer to “vapor trails.”  But the MET is closely connected to UK’s Ministry of Defense, so it’s assumed everything they publish will have some propaganda value.  Why did they choose a picture of old propeller planes forming contrails, not satellite photos like these or modern jet aircraft that better illustrate the scope of the chemtrail program?

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Contrails Creating Clouds

Dr Jim Haywood, Met Office

Ben – Most of us are familiar with the long trails left behind by airplanes as they pass overhead.  But those trails, or contrails as they’re called, can actually give rise to clouds.  We’re joined by Dr. Jim Haywood who’s from the Met office.  Now thank you for joining us, Jim.  My first question really to get a broad idea is how were clouds normally formed?

Jim –   Well, clouds almost invariably form when the air that contains the water vapour cools.  Cooling is almost always initiated by a lifting action.  For example, air flowing over mountains can cause the air to cool to such an extent that the water in it condenses, forming a cloud.  Alternatively, you can have things like cool air undercutting warm air and forcing it to rise in frontal systems associated with low pressure systems in the mid latitudes.  So really, it’s just a case of air being forced to cool, the relative humidity – as meteorologists call it – exceeds 100% and the water in it condenses.

ContrailsBen –   When we see these big lines up in the sky, these contrails from airplanes, what are they actually made of?

Jim –   Obviously, most clouds that we can see from down here are made up of water droplets.  Contrails tend to be made up of ice crystals that grow when the conditions are favourable.

Ben –   How do these then go on to create a cloud?

Jim –   What you can get is – under certain conditions, which is basically cold and moist conditions  – the ice crystals that are initially formed by the aircraft contrail can grow.  It’s a bit like a physics experiment that you probably did at school where you grow crystals of copper sulphate or things in supersaturated solutions.  That’s exactly what’s happening here.  When the conditions are right, it’s cold enough and moist enough up in our atmosphere then the crystals that are initially injected can just grow tremendously and spread with the metrological flow.

Ben –   So we’re not talking about lots of individual particles like we will be for a normal cloud.  This is actually a very large ice crystal that just happens to be light enough to float about.  Is that right?

Jim –   The ice crystals, when they’re initially injected are about a 1000th of a millimetre typically in terms of size.  But as they grow, they can actually get many times that up to about 100 microns.  So, they do form very large crystals which are important in the earth’s radiation budget.

Ben –   These clouds are a bit different than normal clouds.  How do they affect the weather?  Are they rain clouds?  Are we likely to see rain from them or just perhaps a bit of shading or will they not affect us much at all?

Jim –   Well they do affect us in terms of the amount of sunlight that they let through.  That’s quite important.  They tend to reflect sunlight back out to space and lead to a cooling of the weather and consequently, the climate.  But they also trap out going long wave radiation.  So, heat radiation if you like, rather like the greenhouse effect.  So there’s these two competing effects.  You’ve got the reflection of solar radiation or sunlight back out to space and you’ve also got a greenhouse type of effect.  And what’s critical is really the balance between the cooling from the reflection of solar radiation and the warming due to the greenhouse type of effect of these crystals.

Ben –   So if they need particular conditions in which to form, does this mean that certain flight paths are actually more likely to create these clouds and therefore, we’re more likely to have this warming effect or this reduction of sunlight effect in certain areas?

Jim –   Yes, that’s right.  I mean, one of the area that’s particularly good for forming cirrus types of particles – these ice crystals – actually coincides with the air traffic corridors, particularly the one linking North America with Europe.  That’s a particular area that’s good for crystal formation and crystal growth.

Ben –   We’ve had a very, very relevant question from Neil Briscoe.  He said that he heard a while ago – thanks to the 9/11 attacks – when they grounded all the flights, people were able to work out the contrails during daylight hours, helped to prohibit warming by reflecting light back out into space.  But during night time, they actually increased warming.  Is this the same stuff that we’re talking about here?  Does it matter whether it’s day or night?

Jim –   Yes, it does indeed.  It’s exactly what that question is about.  Really, we’re talking about a cooling, if you like from the reflection of sunlight and a warming during the night time which can cause a reduction in what’s called the diurnal temperature range.  After 9/11, there was certainly evidence of a reduction in the diurnal temperature range from a particular study.  But it’s quite difficult to disentangle that signal, if you like from the natural meteorological events that can occur.  And when they looked at it in a little bit more detail, it became almost impossible to distinguish from other events that had nothing to do with 9/11.  You still could see this signal in diurnal temperature range, just due to the natural variability of the atmospheric system.

Ben –   So it may have an impact that we can’t see because it’s no bigger than noise.

Jim –   It’s just difficult to detect.  That’s right.

Ben –   And speaking of detecting it, how do we actually study these things?

Jim – Well, we study it by a number of ways.  We’ve been simulating these contrails and contrails induce cirrus in the state-of-the-science atmospheric models that we use at the Met office and the Hadley Centre for Climate Change.  We’ve also been having a look at various different aircraft measurement campaigns.  I’m involved with an aircraft measuring campaign where we’re trying to create contrails and actually measure the amount of reflected sunlight, and the amount of infrared heat energy that these contrails affect.  So, you can do it from a purely modelling perspective but it’s always better to base it on objective measurements.

Ben –   And, just finally, these contrails obviously tend to stay in one place in the sky.  When they go on to create this cirrus type clouds, do they also stay where they were created or do we find that they drift across the country and have that sort of effect on a slightly wider area?

Jim –   Yes.  We studied one particular contrail that was formed by an Awacs aircraft over the north sea and what we found was although that aircraft had only travelled 1500 kilometres, the area of cloud that it created was actually over 50,000 square kilometres.  This area of cloud – this was created last March – you could see quite clearly being vectored over the UK and lasted for several hours.  It actually lasted for around about 18 hours before the ice crystals started to dissipate.

Ben –   So that’s certainly something to think about next time you’re 30,000 feet above the UK.  You might actually be making it literally cooler for us down on earth in the daytime, possibly a little warmer at night.  That was Jim Haywood.  He’s from the Met Office.

March 2010

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“Global Dimming” documentary video

by qbit on Apr.17, 2010, under In the News, Optical Phenomena, Satellite Imagery

“Global dimming” contains a lot of global warming alarmism with scary music and utterly fails to connect the dots with regard to chemtrails.  What’s important to take from this is the 10-30% global reduction in solar irradiance largely due to aircraft aerosol.

It always astounds me that so many climatologists refuse to entertain the notion that there’s more than just vapor in these “vapor trails.”

I can’t even watch the rest of this overly-dramatic tripe.  When scientists talk about runaway global warming why do they never mention evaporative cooling?  Earth’s surface is 2/3 water.  This isn’t Venus.  Water evaporation must have a limiting effect on greenhouse warming.

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NASA Rocket to Create Clouds Tuesday

by qbit on Sep.14, 2009, under Optical Phenomena

By Clara Moskowitz,
Science News

posted: 14 September 2009 12:21 pm ET

A rocket experiment set to launch Tuesday aims to create artificial clouds at the outermost layers of Earth’s atmosphere.

The project, called the Charged Aerosol Release Experiment (CARE), plans to trigger cloud formation around the rocket’s exhaust particles. The clouds are intended to simulate naturally-occurring phenomena called noctilucent clouds, which are the highest clouds in the atmosphere.

“This is really essentially at the boundary of space,” said Wayne Scales, a scientist at Virginia Tech who will use computer models to study the physics of the artificial dust cloud as it’s released. “Nothing like this has been done before and that’s why everybody’s really excited about it.”

The experiment is the first attempt to create artificial noctilucent clouds. A previous spacecraft, called Aeronomy of Ice in the Mesosphere (AIM), launched in 2007 to observe the natural clouds from space.

CARE is slated to launch Tuesday between 7:30 and 7:57 p.m. EDT (2330 and 2357 GMT) from NASA’s Wallops Flight Facility in Virginia.

Noctilucent means “night shining” in Latin. Although difficult to spot with the naked eye, the clouds are best visible when Earth’s surface is in darkness and sunlight from below the horizon illuminates the high-altitude clouds.

These clouds, also known as polar mesospheric clouds, are made of ice crystals. The natural ones tend to hover around 50 to 55 miles (80 to 90 km) above the Earth. CARE will release its dust particles a bit higher than that, then let them settle back down to a lower altitude.

“What the CARE experiment hopes to do is to create an artificial dust layer,” Scales told SPACE.com. “Hopefully it’s a creation in a controlled sense, which will allow scientists to study different aspects of it, the turbulence generated on the inside, the distribution of dust particles and such.”

CARE is a project of the Naval Research Laboratory and the Department of Defense Space Test Program. The spacecraft will launch aboard a NASA four-stage Black Brant XII suborbital sounding rocket.

Scientists will study its progress from ground based instruments as well as the STP/NRL STPSat-1 spacecraft in Earth orbit. Researchers will track the CARE dust cloud for days or even months to study its behavior and development over time.

Because the optical observations are crucial, the launch can only take place if the weather is clear both at the launch site and at multiple observation stations along the Atlantic coast and in Bermuda.

If CARE cannot launch Tuesday, the team can try again between Sept. 16 and Sept. 20.

070628_night_clouds_02

This image shows one of the first ground sightings of noctilucent clouds in the 2007 season over Budapest, Hungary on June 15, 2007. Credit: Veres Viktor

080901-iran-cloud-02

Noctilucent clouds over Mt. Sabalan, a 15,784 ft extinct volcano in northwestern Iran. Credit: Siamak Sabet

070411_aim_clouds_02

Noctilucent clouds over northern Europe. Credit: Pekka Parvianien.

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Surprise: “Noctilucent clouds” may be human made.

by qbit on Jul.29, 2009, under Optical Phenomena

Comet likely culprit in Tunguska blast
Clouds over London following the event are similar to those formed from today’s shuttle plumes
Web edition : Tuesday, July 28th, 2009

Night-shining clouds created after space shuttle launches may offer clues into the cause of the Tunguska event, a mysterious blast which rocked southern Siberia more than a century ago.

Thin clouds have appeared at abnormally high altitudes over polar regions following space shuttle launches on several occasions in the past decade. These noctilucent, or night-shining, clouds typically occur in summer and lie at altitudes of about 85 kilometers, in a layer of the atmosphere called the thermosphere, says Michael C. Kelley, an atmospheric physicist at Cornell University. Kelley and his colleagues suggest in the July 28 Geophysical Research Letters that data gleaned from analyses of these high-flying clouds, as well as knowledge about the speed at which shuttle exhaust wafted to polar regions, now hint that the Tunguska blast of June 1908 (SN: 6/21/08, p. 5) resulted from a comet slamming into Earth’s atmosphere.

Each launch of a space shuttle, which burns a combination of liquid hydrogen and liquid oxygen as fuel, pumps about 300 metric tons of water vapor into the atmosphere at altitudes between 100 and 115 kilometers. Soon after the January 16, 2003, launch of the shuttle Columbia, a liftoff that took place just after the height of summer in the Southern Hemisphere, noctilucent clouds appeared over Antarctica. Similarly, a widespread display of the night-shining clouds showed up over Alaska two days after the shuttle Endeavour blasted off on August 8, 2007. Previous studies show that in both instances those clouds included material from the shuttle plumes.

“Conventional wisdom says that the plumes shouldn’t reach the poles that quickly, but they do,” Kelley notes. So sustained high-altitude winds must be carrying the plumes to the poles.

Michael S. Stevens, a research physicist at the Naval Research Laboratory in Washington, D.C., agrees: Experiments show that “winds can be strong at these altitudes, but they’re not well understood.”

Using data based on shuttle plume movement, the researchers suggest that the Tunguska blast could have been responsible for unusually bright noctilucent clouds over Europe soon thereafter. The likely composition of those clouds further suggests that a comet caused the blast.

Some of the thickest and brightest noctilucent clouds ever observed — ones that cast enough light to read a newspaper in the middle of the night — appeared over Europe on July 1, 1908, Kelley says. Not coincidentally, he and his colleagues argue, the Tunguska blast occurred over southern Siberia about 22 hours earlier. The team’s models suggest that winds and diffusion could have transported material from the site of the blast to the skies over London, a distance of about 5,000 kilometers, in little more than a day.

Scientists at the time suggested that the night-shining clouds over London were made of meteoritic dust. But those aerosols are typically too small to reflect sunlight efficiently, Kelley argues, suggesting the clouds above Europe were made of ice crystals. This assumption, along with the new analysis of shuttle plume movement, strongly suggests that the object that blazed into the atmosphere and disintegrated above Siberia was a moisture-rich comet rather than a relatively dry asteroid.

“That’s an interesting idea, and worth considering,” Stevens says. In an alternate scenario, he notes, rather than the moisture being transported to Europe and then coalescing into clouds, the clouds may have formed over Siberia and then been transported to the west.

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“Weird looking cloud”

by qbit on Feb.15, 2009, under In the News, Optical Phenomena

HEY DUMBASS, ITS CALLED A CHEMBOW

A weird-looking cloud sporting the colors of the rainbow appeared to many in the Dallas-Fort Worth Metroplex early Thursday afternoon.The cloud stayed in the southeastern sky for several minutes, but was obscured by other clouds at times. NBC 5 Meteorologist James Aydelott offered one possible explanation, saying that the sun was hitting the cloud at just the right angle, similar to a phenomenon known as “sun dogs,” causing the colorful display. He also said he had never seen a cloud like this before.

Perfectly normal, nothing to see here, move along.

Perfectly normal, nothing to see here, move along.

Interesting discussion about this here:
http://www.chemtrailcentral.com/forum/msg86828.html

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More chembows

by qbit on Feb.03, 2009, under Optical Phenomena

I see these on a regular basis now in Michigan. See previous post on diffraction and chembows.

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What are “chembows?”

by qbit on Jan.25, 2009, under Optical Phenomena, What are they?

If you’ve been paying attention to chemtrails, you may have observed rainbow smearing (diffraction) of light reflected off them.  Dark sunglasses can bring the subtle rainbows into the dynamic range of the human eye.  Chembows are often visible when the sunlight reflects at approximately 45• angle to the chemtrail.  Wikipedia entry on diffraction

A popular chembow image. Notice how only the wispy remnants of the chemtrail diffract the sunlight, <i>not</i> the nearby clouds.

A popular chembow image. Notice how only the wispy remnants of the chemtrail diffract the sunlight, not the clouds.

Diffraction is a quantum interaction between photons of light and edges of atoms.  When metallic surfaces have features smaller than a wavelength of visible light (nanometer scale),  different wavelengths will be reflected at different angles.  When features are ordered in a linear pattern (such as on a DVD optical disc), a rainbow will appear.

Illustration of white light diffracting off a metallic "diffraction grating"

Illustration of white light diffracting off a metallic diffraction grating

Diffraction off the bottom of a metallic optical disc.

In the rain, or other atmospheric conditions where water droplets are large enough, rainbows appear due to refraction.  Atmospheric refraction (such as from a rainbow in a rainstorm) is a similar phenomenon to chemtrail diffraction.  Its important to note, however, that rainbows can be seen in light reflected off chemtrails, not only refracted from behind, which may occur under other atmospheric conditions, such as the presence of large ice crystals or droplets.

Refraction thru a prism (or water droplet of sufficient size). Refraction occurs when light passes thru a surface into a material with different <i>index of refraction</i>

Refraction thru a prism (or water droplet of sufficient size). Refraction occurs when light passes thru a surface into a material with different index of refraction

More examples of chembows:

2556642904_a202f7cf86

Dark sky indicates reduced exposure, necessary to bring rainbow into dynamic range of the sensor.

Filamentous wisps may indicate presence of heavier-than-water particulate aerosol.

Filamentous wisps may indicate presence of heavier-than-water particulate aerosol. Pink and green dominate the rainbow, matching emission spectra of barium.

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