JazzRoc versus “Chemtrails”

Contrail Facts and “Chemtrail” Fictions

Posts Tagged ‘trade wind

6 Porkies

with 4 comments

PAGE CONTENTS

6 PORKIES – AEROSOLS – THE ATMOSPHERE – THE WMO – ATMOSNAPS

Don’t forget my other pages, links and comments are one click away at the top right of the page…

 

“PORK PIE” = “LIE”  – Cockney rhyming slang. 

porkpie

6 PORKIES

“Obviously your alleged credentials are fraud” – has your short-term memory passed away? ONE.

“A true person of Science would step forward and lay all questions to rest” – ditto, and I have. Check my comments here. Check http://www.contrailscience.com. Check http://www.myspace.com/jazzroc TWO.

“You do nothing” – I COULD start pasting again… THREE.

“It is safe to assume that people’s claims must have basis” – assuming is the only action you do. Why not educate yourself in science? FOUR.

“I’d like nothing more than for someone to prove nothing is going on” – FIVE.

“You are by far not only a fraud but a coward as well” – GIANT PORKY NUMBER SIX.

AEROSOLS

What a great porky this one is!

The non-scientific word-association goes aerosol – hair spray – sprayers (truly inspirational!)

aerosol-can-2

TO THIS:

YouTube_-_Documentary_Validates_Chemtrails_and_Weather_Warfare-20090725-091314

But never a thought to CHECKING UP what the REAL MEANING (scientific meaning) of aerosol ACTUALLY IS:

Aerosol – from Wikipedia, the free encyclopedia
 
Aerosol – contamination in northeastern India and Bangladesh.
Technically, an aerosol is a suspension of fine solid particles or liquid droplets in a gas. Examples are smoke, oceanic haze, air pollution, smog and CS gas. In general conversation, aerosol usually refers to an aerosol spray can or the output of such a can.
The word aerosol derives from the fact that matter “floating” in air is a suspension (a mixture in which solid or liquid or combined solid-liquid particles are suspended in a fluid). To differentiate suspensions from true solutions, the term sol evolved – originally meant to cover dispersions of tiny (sub-microscopic) particles in a liquid.
With studies of dispersions in air, the term aerosol evolved and now embraces both liquid droplets, solid particles, and combinations of these.

Workplace exposure
Concentrated aerosols from substances such as silica, asbestos, and diesel particulate matter are sometimes found in the workplace and have been shown to result in a number of diseases including silicosis and black lung. Respirators can protect workers from harmful aerosol exposure. In the United States the National Institute for Occupational Safety and Health certifies respirators through the National Personal Protective Technology Laboratory to ensure that they protect workers and the public from harmful airborne contaminants.

Effect on climate
Aerosols over the Amazon each September for four burning seasons (2005 through 2008). The aerosol scale (yellow to dark reddish-brown) indicates the relative amount of particles that absorb sunlight. Anthropogenic aerosols, particularly sulfate aerosols from fossil fuel combustion, exert a cooling influence on the climate which partly counteracts the warming induced by greenhouse gases such as carbon dioxide. This effect is accounted for in many climate models. Recent research, as yet unconfirmed, suggests that aerosol diffusion of light may have increased the carbon sink in the earth’s ecosystem.

Recent studies of the Sahel drought and major increases since 1967 in rainfall over the Northern Territory, Kimberley, Pilbara and around the Nullarbor Plain have led some scientists to conclude that the aerosol haze over South and East Asia has been steadily shifting tropical rainfall in both hemispheres southward.

The latest studies of severe rainfall declines over southern Australia since 1997 have led climatologists there to consider the possibility that these Asian aerosols have shifted not only tropical but also mid-latitude systems southward.

Oxides of nitrogen (NOx) in the atmosphere are a form of pollution which can give rise to smog and act as a greenhouse gas. Their persistence in the atmosphere is affected by aerosol droplets of water.
In 1964 long chain fatty acids, either naturally produced from marine organisms dispersed into the atmosphere by wave action or man-made, were found to coat these droplets. In 2006 there was a study of the effect of the LCFA on the persistence of NOx, but the long term implications, although thought to be significant, have yet to be determined.

So AEROSOL means this:

aerosol_clouds
Or this:
aerosol-692
A REALTIME study of aerosol presence (made by satellite) all over the world may be obtained here, and here is a representative image, from which you can see the satellite passes 90 minutes apart.
aersl_omi_2009

There is a video made over a fortnight showing the main aerosol action occurs travelling westward on a line passing through BANGLADESH and the SAHARA DESERT. It is MAN-MADE – the consequence of many hundreds of millions of humans living close to the poverty line…  slash-and-burn, cooking fires, forest fires, vegetable farming decomposition, volcanoes…

No aircraft contrails are found anywhere NEAR this line…

So much for the “chemtrailers” and their “the NWO is poisoning the whole world” theory…

rd-table

THE ATMOSPHERE

What is it?

atmosphereearth

It’s a mixture of invisible element and compound gases; nitrogen, oxygen, carbon dioxide, water vapour, argon, neon, and trace amounts of other inert gaseous elements. This mixture keeps us in a healthy condition, and imbalance in this mixture can poison and/or kill us. We would all prefer to be at Standard Temperature and Pressure, which is 20 deg C (70 deg F) and 1000 millibars (14.7 lb/in2).

Standard Temperature and Pressure occur at Sea Level, but the atmosphere may reach up to 200Km or more (the INTERNATIONAL SPACE STATION orbits at 400Km and you can bet there’s very little atmosphere, if any, at that height!) The following diagram is a graph of atmospheric pressure against height over sea level (altitude). The space station height is three graph-heights higher than the graph below.

pressure_altitude.jpg

There is an asymptotic fall-off of pressure with altitude which is easy to see. This, when combined with the concomitant drop in temperature lends weight to the understanding that the stratosphere cannot bear much loading of contrail ice before it saturates, and cannot absorb more.

The region just immediately higher than the tropopause (at approximately 26,000 feet to 39,000 feet) is the region where passenger aircraft fly, for reasons of safety and economy.

The pressure above the tropopause is one-fifth that at sea level, but at the high cruising speed of 550 miles per hour, there is sufficient dynamic lift for safe and stable flight.

This region is the CAUSE of the “chemtrail” controversy, for it is COLD, STABLE, and INCAPABLE of absorbing large amounts of combustion steam as water vapor. As a consequence this steam cools to microscopically-fine ice crystals, which form – TRAILS behind the aircraft.

And the following is a diagram of air dewpoint and temperature plotted against height above sea level (altitude).

humidity.jpg

If you look at the dewpoint line (on left) you can see it move continually leftward with increase in height above sea level. This powerfully indicates that with increasing height, the atmosphere is increasingly incapable of absorbing the exhaust water formed by burning kerosine in gas turbines.

Looking at the temperature (lapse rate) line on the right, you can see that it moves leftward with increase in height above sea level, until it reaches the tropopause, where it starts to edge to the right again. You can see that after the tropopause the atmosphere gets WARMER with increasing height. The concave shapes to both dewpoint and temperature here indicate some energy input – either solar ‘focusing’ from tropospheric clouds, or jet stream mixing energy – it is hard to guess.

Another couple of points. This chart was obviously made on a cold day; the sea level temperature is just sub-zero. However, two hundred metres higher, and the air temperature is five degrees higher. Bumps and dips in these two lines show where you may infer the presence of clouds.

top_of_atmosphere

There is much more to learn about our atmosphere than I have given here, but I can heartily recommend this link to the UK’s Met Office.

After that you can answer these questions (can’t you!).

atm-qs.jpg

As further confirmation I strongly recommend AtOptics

atopticsatm.

And a word to the “wise”. There is a lot of scuttlebutt going around which says “Global Warming is just a myth started by our duplicitous governments as a means of extracting additional taxes”. Well I remember a time when it was thought we were headed directly for a new ice age.

(This was just a journalistic ruse. The next Ice Age will occur approximately 16,000 years from the present.)

Since then, it is true that government funds are available for the investigation of GW to the detriment of other research, and that horrible thing “political correctness” has raised its ugly head above the horizon, but the facts are too numerous to mention that the climate is warming, but also that other facts remain unmentioned, which leaves a question of politics…

greenhouse_effect

See “Global Warming is a Myth” under G in this blog.

https://jazzroc.wordpress.com/2008/11/03/19-global-dimming/

gw

THE WORLD METEOROLOGICAL ORGANIZATION

One of the major purposes of the World Meteorological Organization (WMO), as laid down in its Convention, is “To facilitate worldwide cooperation in the establishment of networks of stations for the making of meteorological observations as well as hydrological and other geophysical observations related to meteorology, and to promote the establishment and maintenance of centres charged with the provision of meteorological and related services”.

Accordingly, WMO Members operate, in a coordinated manner, complex networks in space, the atmosphere, on land and over oceans. In 2007, Members decided to work towards enhanced integration of both the WMO Global Observing System (GOS) and WMO co-sponsored observing systems such as the Global Ocean Observing System (GOOS), Global Terrestrial Observing System (GTOS) and Global Climate Observing System (GCOS). This concept is called the WMO Integrated Global Observing Systems (WIGOS).

  weather balloon

Currently, more than 10000 manned and automatic surface weather stations, 1000 upper-air stations, over 7000 ships, more than 100 moored and 1000 drifting buoys, hundreds of weather radars and over 3000 specially equipped commercial aircraft measure key parameters of the atmosphere, land and ocean surface every day. The space-based component of the WMO Observing System contains operational polar-orbiting and geostationary satellites and also R&D environmental satellites complementing ground-based global observations. These activities are coordinated within the Global Observing System (GOS) of the World Weather Watch (WWW) of WMO. Several WMO Programmes sponsor or participate in the operation of several global observing systems. Other global observing systems, e.g. the global hydrological networks (WHYCOS), function principally on a national or regional level.

Observation programmes such as the Global Climate Observing System (GCOS) and the Global Ocean Observing System (GOOS) will continue to play a major role in improving the collection of required data for the development of climate forecasts and climate change detection. WMO’s Global Atmosphere Watch (GAW) provides data for scientific assessments and for early warnings of changes in the chemical composition and related physical characteristics of the atmosphere that may have adverse affects upon our environment. Through its Instruments and Methods of Observation Programme (IMOP), WMO ensures that meteorological instruments, including manual and automatic ground-based stations and space-based observing systems, are accurate and provide standardized data.

WMO monitoring and observing systems will be a core component of the Global Earth Observation System of Systems (GEOSS), aimed at developing a comprehensive, coordinated and sustained Earth observation system of systems to understand and address global environmental and economic challenges.

ATMOSNAPS

This is, of course, a silly word coined by me to introduce these pictures of Earth’s atmosphere which have been taken by some of the NASA Space Shuttle astronauts from the International Space Station.

I find them most stimulating and interesting. We spend all our time with a “flat-earther” viewpoint, looking up at clouds and failing to see them for what they truly are.

Moment of Launch - "the twang's the thang!"

Moment of Launch - "the twang's the thang!"

Shuttle lift-off at Cape Kennedy

Shuttle lift-off at Cape Kennedy

Out on a limb...

Out on a limb...

A massive cumulo-nimbus from above...

A massive cumulo-nimbus from above...

A Saharan sandstorm leaves the West Coast of Africa

A Saharan sandstorm leaves the West Coast of Africa

Eddies form in Cirrus clouds passing over a Mediterranean isle

Eddies form in Cirrus clouds passing over a Mediterranean isle

A sunset from space...

A sunset from space...