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originally posted by: mrthumpy
originally posted by: intrptr
originally posted by: mrthumpy
originally posted by: intrptr
a reply to: Soylent Green Is People
Thanks for agreeing with me, round about wise. The water in the atmosphere needs particulates to begin to condense on, that particulate is the exhaust chemical compounds and soot that exits the jet engine.
The exhaust particulate isn't actually required though, there's enough condensation nuclei in the atmosphere already
Yah, from the last ten thousand jet flybys. Not required, lulz.
Right because before jets there were no clouds
lulz
originally posted by: intrptr
originally posted by: mrthumpy
originally posted by: intrptr
originally posted by: mrthumpy
originally posted by: intrptr
a reply to: Soylent Green Is People
Thanks for agreeing with me, round about wise. The water in the atmosphere needs particulates to begin to condense on, that particulate is the exhaust chemical compounds and soot that exits the jet engine.
The exhaust particulate isn't actually required though, there's enough condensation nuclei in the atmosphere already
Yah, from the last ten thousand jet flybys. Not required, lulz.
Right because before jets there were no clouds
lulz
'Clouds' aren't pollution.
originally posted by: intrptr
a reply to: Soylent Green Is People
The water in the atmosphere needs particulates to begin to condense on, that particulate is the exhaust chemical compounds and soot that exits the jet engine.
originally posted by: Soylent Green Is People
originally posted by: mrthumpy
originally posted by: intrptr
a reply to: Soylent Green Is People
Thanks for agreeing with me, round about wise. The water in the atmosphere needs particulates to begin to condense on, that particulate is the exhaust chemical compounds and soot that exits the jet engine.
The exhaust particulate isn't actually required though, there's enough condensation nuclei in the atmosphere already
True, but not all of the visible ice crystals in a contrail are condensing on particulates from jet exhaust. That jet exhaust could be a seed that starts a contrail, but once the contrail starts (and under the right conditions for persistence), it is the ice crystals themselves that become a nucleation point...
...i.e., ice crystals in a persistent and spreading contrail nucleate onto existing ice crystals in the contrail (in a chain reaction) and other ambient particulates, NOT onto the soot from burnt jet fuel.
originally posted by: mrthumpy
originally posted by: Soylent Green Is People
originally posted by: mrthumpy
originally posted by: intrptr
a reply to: Soylent Green Is People
Thanks for agreeing with me, round about wise. The water in the atmosphere needs particulates to begin to condense on, that particulate is the exhaust chemical compounds and soot that exits the jet engine.
The exhaust particulate isn't actually required though, there's enough condensation nuclei in the atmosphere already
True, but not all of the visible ice crystals in a contrail are condensing on particulates from jet exhaust. That jet exhaust could be a seed that starts a contrail, but once the contrail starts (and under the right conditions for persistence), it is the ice crystals themselves that become a nucleation point...
...i.e., ice crystals in a persistent and spreading contrail nucleate onto existing ice crystals in the contrail (in a chain reaction) and other ambient particulates, NOT onto the soot from burnt jet fuel.
I know. My point is that the initial condensation would still take place and a contrail would still form without the particulates in the exhaust as there are plentiful cloud condensation nuclei naturally in the atmosphere. Even a hydrogen powered jet with nothing other than water in the exhaust will still form a contrail.
originally posted by: intrptr
a reply to: Soylent Green Is People
The water in the atmosphere needs particulates to begin to condense on, that particulate is the exhaust chemical compounds and soot that exits the jet engine.
originally posted by: intrptr
originally posted by: mrthumpy
originally posted by: intrptr
a reply to: Soylent Green Is People
Thanks for agreeing with me, round about wise. The water in the atmosphere needs particulates to begin to condense on, that particulate is the exhaust chemical compounds and soot that exits the jet engine.
The exhaust particulate isn't actually required though, there's enough condensation nuclei in the atmosphere already
Yah, from the last ten thousand jet flybys. Not required, lulz.
Aerosols interact both directly and indirectly with the Earth's radiation budget and climate. As a direct effect, the aerosols scatter sunlight directly back into space. As an indirect effect, aerosols in the lower atmosphere can modify the size of cloud particles, changing how the clouds reflect and absorb sunlight, thereby affecting the Earth's energy budget. Aerosols also can act as sites for chemical reactions to take place (heterogeneous chemistry). The most significant of these reactions are those that lead to the destruction of stratospheric ozone. During winter in the polar regions, aerosols grow to form polar stratospheric clouds. The large surface areas of these cloud particles provide sites for chemical reactions to take place. These reactions lead to the formation of large amounts of reactive chlorine and, ultimately, to the destruction of ozone in the stratosphere. Evidence now exists that shows similar changes in stratospheric ozone concentrations occur after major volcanic eruptions, like Mt. Pinatubo in 1991, where tons of volcanic aerosols are blown into the atmosphere (Fig. 1).
Volcanic Aerosol Three types of aerosols significantly affect the Earth's climate. The first is the volcanic aerosol layer which forms in the stratosphere after major volcanic eruptions like Mt. Pinatubo. The dominant aerosol layer is actually formed by sulfur dioxide gas which is converted to droplets of sulfuric acid in the stratosphere over the course of a week to several months after the eruption
Desert Dust The second type of aerosol that may have a significant effect on climate is desert dust. Pictures from weather satellites often reveal dust veils streaming out over the Atlantic Ocean from the deserts of North Africa. Fallout from these layers has been observed at various locations on the American continent. Similar veils of dust stream off deserts on the Asian continent. The September 1994 Lidar In-space Technology Experiment (LITE), aboard the space shuttle Discovery (STS-64), measured large quantities of desert dust in the lower atmosphere over Africa
Human-Made Aerosol The third type of aerosol comes from human activities. While a large fraction of human-made aerosols come in the form of smoke from burning tropical forests, the major component comes in the form of sulfate aerosols created by the burning of coal and oil. The concentration of human-made sulfate aerosols in the atmosphere has grown rapidly since the start of the industrial revolution. At current production levels, human-made sulfate aerosols are thought to outweigh the naturally produced sulfate aerosols. The concentration of aerosols is highest in the northern hemisphere where industrial activity is centered. The sulfate aerosols absorb no sunlight but they reflect it, thereby reducing the amount of sunlight reaching the Earth's surface. Sulfate aerosols are believed to survive in the atmosphere for about 3-5 days.
originally posted by: intrptr
All types from all sources for decades.
We provide an overview of geoengineering by stratospheric sulphate aerosols. The state of understanding about this topic as of early 2008 is reviewed, summarizing the past 30 years of work in the area, highlighting some very recent studies using climate models, and discussing methods used to deliver sulphur species to the stratosphere
This study describes an approach to cooling the planet, which goes back to the mid-1970s, when Budyko (1974) suggested that, if global warming ever became a serious threat, we could counter it with airplane flights in the stratosphere, burning sulphur to make aerosols that would reflect sunlight away.
An alternative would be to use a precursor gas that is quite long-lived in the troposphere but oxidizes in the stratosphere and then allow the Earth's natural transport mechanisms to deliver that gas to the stratosphere, and diffuse it prior to oxidation. OCS might serve as a natural analogue to such a gas (Turco et al. 1980), although it is carcinogenic and a greenhouse gas.
It might also be possible to create a custom molecule that breaks down in the stratosphere that is not a carcinogen, but using less reactive species would produce a reservoir species that would require years to remove if society needs to stop production. Problems with this approach would be reminiscent of the climate impacts from the long-lived chlorofluorocarbons (CFCs), although lifetimes are shorter.
Our generic platform is a jet-fighter-sized aircraft carrying a payload of 10 metric tons of finely divided aerosol, or an equivalent precursor mass, to be distributed evenly over a 2500 km flight path during an 4-hour flight (while few aircraft are currently capable of sustained flight at stratospheric heights, platform design issues are neglected at this point). The initial plume cross section is taken to be 1 m2, which is consistent with the dimensions of the platform. Note that, with these specifications, a total aerosol mass injection of 10 Tg of particles per year would call for 1 million flights, and would require several thousand aircraft operating continuously in the foreseeable future. To evaluate other scenarios or specifications, the results described below may be scaled to a proposed fleet or system.
Enhancing aircraft fuel with added sulphur compounds (H2S, Sn) could increase the particle mass in a jet wake. It is well established that ultrafine sulphate particles are generated copiously in jet exhaust streams during flight
If we imagine enhanced jet fuel sulphur contents of 5 per cent by weight (10–100 times current amounts) for geoengineering purposes, then the annual consumption of approximately 50 Tg of such fuel during stratospheric flight (approx. half the amount used by current commercial aviation) could emit up to 2.5 Tg of sulphur that would eventually generate roughly 10 Tg of sulphate aerosol. The total number of particles emitted—for Ep∼1×1017 kg−1 fuel—would amount to approximately 5×1027. This number, uniformly dispersed over a 10-km thick layer from 15 to 25 km, yields an average concentration of approximately 1×103 cm−3 with a particle radius of roughly 0.06 μm; in other words, an ideal geoengineered solar shield. These estimates (i) assume no unexpected chemistry or microphysics in the early wake that would alter the emission factor significantly, (ii) allow for an ideal distribution of sulphate mass among the particles, and (iii) ignore coagulation following emission.
You seem to have a habit of blaming everything on aircraft exhaust.
originally posted by: intrptr
a reply to: network dude
You seem to have a habit of blaming everything on aircraft exhaust.
That is the topic...
but why I don't engage with you anymore about it. We been all over this road before. I say something and you put words in my mouth.
late
originally posted by: fema1
Well here is a bomb shell from the CFR about BS on climate change for an excuse to use Aerosols!
Where could these planes possibly land, is the real question...
originally posted by: DJW001
a reply to: turbonium1
Where could these planes possibly land, is the real question...
There's this place called "Asia." Try using Google Maps.
originally posted by: turbonium1
Planes would not be flying in every direction, going nowhere,
Some of these planes are going directly west, to the vast Pacific Ocean...!!
Where could these planes possibly land, is the real question...
They are flying over an international airport, but none of them need more fuel in crossing the Pacific!
Why are the planes above the city, all the time? No reason, flying over cities is just for fun!!
originally posted by: Zaphod58
a reply to: turbonium1
Contrary to what you apparently believe, flying from point A to point B in a straight line is NOT the most efficient way to get somewhere. The most efficient way to get there is to fly the great circle route. That means when flying to Beijing, you fly up the West Coast of the US, circle under Alaska, down the West Coast of Russia, and into China. It does NOT mean flying straight out over the Pacific, over Hawaii, to China. If they flew that route, they WOULD need more fuel.