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Really? Where is the evidence for that? ditto - what is the mechanism by which "natural" cirrus is "supplanted"?? how is that?? clearly their inception is different - but what is the evidence that the behaviour after that is any different? In what way are they different? I have never seen any reason being given for deliberate formation of cirrus aviaticus at all - where did yuo get this from? so what are the references for this conclusion? Destroying all clouds?? Really? so no rain? How will that cool the planet? Again - where are the references?
So what else where the rockets were not too visible?
The stratosphere is also much drier than the troposphere, and clouds rarely form at this level.
Subsonic aircraft fly in the troposphere and lower stratosphere, whereas supersonic aircraft fly in the stratosphere 80-85% of the time, with cruise altitudes several kilometers above those of subsonic aircraft.
Comparisons of aircraft cruise altitudes with mean tropopause heights has led to estimates for stratospheric release of 20-40% of total emissions (Hoinka et al., 1993; Baughcum, 1996; Schumann, 1997; Gettleman and Baughcum, 1999).
In the future, aircraft with more fuel-efficient engines will produce lower exhaust temperatures for the same concentration of emitted water vapor, hence will tend to cause contrails at higher ambient temperatures and over a larger altitude range
Aircraft generate far less aerosol than that emitted and produced at the Earth's surface or by strong volcanic eruptions. Aircraft emissions injected directly at 9- to 12-km altitudes are more important than similar surface emissions because of longer atmospheric residence times in the upper troposphere.
Regions of ice-supersaturation vary with time and location and are estimated to cover an average of 10 to 20% of the Earth's surface at mid-latitudes. Ice-supersaturation in these regions is often too small to allow cirrus to form naturally, so aircraft act as a trigger to form cirrus clouds
Originally posted by Uncinus
reply to post by luxordelphi
Radiative Forcing from jet emissions is a very small part of total man-made radiative forcing.
I guess that means that with conditions under which natural clouds would have formed contrails form instead because they form sooner.
Yes, and, in forming, prevent the formation of natural clouds.
www.nature.com...
Contrail cirrus exist alongside and interact with natural clouds and, depending on their overlap with natural clouds, can increase overall cloud coverage
It's not so much a matter of chemistry but I understand what you mean about that second part. It's sort of like how it's not specifically stated anywhere that chaff and SRM are not really complementary.
I'm not a chemist but that's what I get from reading the material even though it never gets specifically stated all in one paper.
www.agu.org...
Mixing of moist environmental air and vapor depleted contrail air produced localized regions of supersaturation along the contrail periphery, where crystals grew to several hundred microns at about 0.1 µm s−1 These particles could then fall from the contrail into the vapor rich, undepleted, supersaturated environment below. As heavier crystals left the contrail, others moved into the regions of ice supersaturation. Precipitation trails developed as this process continued over time.
lidarmax.altervista.org...
The main cluster of Fig.1 could thus be attributed to "aged" contrails, dominated by ice crystals that were larger than a few microns. This interpretation was supported by the presence in the time-height-backscatter plots of virgas or diffuse structures around the core of the majority of these contrails
eprints.whiterose.ac.uk...
The development of virga falling from contrails is a manifestation of a favorable environment for growth and the development of contrail cirrus (T1, T4, and T10). With a sustained ice-supersaturated environment, some contrail microphysical properties become similar to those of natural cirrus, for example, concentrations of ice crystals larger than 100 μm in diameter are of the order of 10–100 l−1, and the habits are bullet rosettes (T5).
So SRM...solar radiation management...the deliberate act of trying to reflect sunlight away from earth...in order to combat global warming...is also deliberately or ignorantly or as a side-effect, practised through jet emissions.
www.nature.com...
Aviation makes a significant contribution to anthropogenic climate forcing. The impacts arise from emissions of greenhouse gases, aerosols and nitrogen oxides, and from changes in cloudiness in the upper troposphere.
airquality.ucdavis.edu...
Aviation contributes to climate change by increasing atmospheric radiative forcing through the emission of gases and aerosols and changing cloud abundance.
www.tiaca.org...
Aviation emissions contribute to the radiative forcing (RF) of climate. Of importance are emissions of carbon dioxide (CO2), nitrogen oxides (NOx), aerosols and their precursors (soot and sulphate), and increased cloudiness in the form of persistent linear contrails and induced-cirrus cloudiness.
Well, yes. Just as pretty much the entire environment is affected to one degree or another by a whole lot of things that humans do. Unfortunately (or not, depending on your point of view), it's what we do.
And if these parameters are present then the stratosphere is impacted.
Originally posted by Uncinus
reply to post by luxordelphi
Radiative Forcing from jet emissions is a very small part of total man-made radiative forcing.
Besides the uncertainty due to the treatment of contrail cirrus, our radiative-forcing estimates are also affected particularly by uncertainties related to the model’s representation of upper-tropospheric humidity and clouds. Clouds are influenced by small-scale processes that cannot be resolved by a large-scale climate model and which therefore need to be parametrized. The representation of clouds is a major source of uncertainty in climate simulations. The same problems also affect the representation of contrail cirrus.
The uncertainty of the radiative-forcing estimates should be evaluated from independent studies based on different models and contrail-cirrus parameterizations. Reducing the uncertainty in the evaluation of contrail-cirrus radiative forcing requires more and better observational data sets.
Originally posted by luxordelphi
reply to post by Aloysius the Gaul
Really? Where is the evidence for that? ditto - what is the mechanism by which "natural" cirrus is "supplanted"?? how is that?? clearly their inception is different - but what is the evidence that the behaviour after that is any different? In what way are they different? I have never seen any reason being given for deliberate formation of cirrus aviaticus at all - where did yuo get this from? so what are the references for this conclusion? Destroying all clouds?? Really? so no rain? How will that cool the planet? Again - where are the references?
The strange questions and bizarre statements just go on and on. Failure to observe and failure to read links has not served you well.
So what else where the rockets were not too visible?
This one on SRM I'm going to address because it hasn't really been covered at all as far as how jet emissions affect the stratosphere and affecting the stratosphere affect everything else.
So SRM...solar radiation management...the deliberate act of trying to reflect sunlight away from earth...in order to combat global warming...is also deliberately or ignorantly or as a side-effect, practised through jet emissions.
www.ipcc.ch...
The stratosphere is also much drier than the troposphere, and clouds rarely form at this level.
Subsonic aircraft fly in the troposphere and lower stratosphere, whereas supersonic aircraft fly in the stratosphere 80-85% of the time, with cruise altitudes several kilometers above those of subsonic aircraft.
Comparisons of aircraft cruise altitudes with mean tropopause heights has led to estimates for stratospheric release of 20-40% of total emissions (Hoinka et al., 1993; Baughcum, 1996; Schumann, 1997; Gettleman and Baughcum, 1999).
In the future, aircraft with more fuel-efficient engines will produce lower exhaust temperatures for the same concentration of emitted water vapor, hence will tend to cause contrails at higher ambient temperatures and over a larger altitude range
Aircraft generate far less aerosol than that emitted and produced at the Earth's surface or by strong volcanic eruptions. Aircraft emissions injected directly at 9- to 12-km altitudes are more important than similar surface emissions because of longer atmospheric residence times in the upper troposphere.
Regions of ice-supersaturation vary with time and location and are estimated to cover an average of 10 to 20% of the Earth's surface at mid-latitudes. Ice-supersaturation in these regions is often too small to allow cirrus to form naturally, so aircraft act as a trigger to form cirrus clouds
So in the case of the stratosphere and whether or not it is being affected, the proof would be: see plane; see plane fly. And if these parameters are present then the stratosphere is impacted.
I guess that means that with conditions under which natural clouds would have formed contrails form instead because they form sooner.
But when natural cirrus already exist contrails do not somehow suck the moisture out of the ice crystals and cause the natural clouds to evaporate.
Therefore, contrail cirrus have the potential to modulate the optical properties of natural clouds, delaying their onset and replacing them, which may partly offset the direct climate impact of contrail cirrus.
This potential for heterogeneous nuclei to cause ice formation at ice supersaturations that are relatively low compared to those needed to freeze sulfate particles leads to concern about the role of aircraft exhaust in modifying ambient clouds (Jensen and Toon, 1997).
Thus, cirrus clouds have a net warming effect on the earth's climate (Hartmann et al, 1992; Chen et al, 2000). It follows then that the most effective way to increase OLR may be to reduce the cloud cover of the highest, coldest cirrus clouds.
One method for how this goal might be accomplished is described in MF2009. They suggested "seeding" cirrus clouds with efficient ice nuclei that would out-compete the natural ice nuclei for water vapor.
Contrail cirrus exist alongside and interact with natural clouds and, depending on their overlap with natural clouds, can increase overall cloud coverage.
Only part of the contrail/contrail-cirrus coverage leads to an increase in overall cloud coverage.
The change in cirrus coverage, calculated by vertically overlapping all ice clouds in a column, confirms that the natural-cirrus coverage is decreased owing to the presence of contrail cirrus.
Furthermore, in the main contrail-cirrus areas of North America and Europe, the optical depth of natural clouds is significantly (at the 95% significance level) reduced by up to 10% owing to the presence of contrail cirrus.
It's sort of like how it's not specifically stated anywhere that chaff and SRM are not really complementary.
Since the discussion has been about your statement that contrail cirrus can lead to drought conditions because, unlike natural cirrus, they for some unstated purpose do not produce ice crystals which precipitate to lower levels. This study would seem to indicate otherwise:
Thus, cirrus clouds have a net warming effect on the earth's climate (Hartmann et al, 1992; Chen et al, 2000). It follows then that the most effective way to increase OLR may be to reduce the cloud cover of the highest, coldest cirrus clouds.
One method for how this goal might be accomplished is described in MF2009. They suggested "seeding" cirrus clouds with efficient ice nuclei that would out-compete the natural ice nuclei for water vapor.
As noted above, higher fall speeds will result in shorter cloud lifetimes, less cloud coverage, lower ice water paths and lower cloud optical depths.
2.2 Reducing cloud cover for the coldest cirrus clouds...Cirrus clouds might be modified by seeding aerosol at any temperature, provided the natural ice nuclei, whether heterogeneous or homogenous, activates at a RH, well above the RH, threshold of the seeding aerosol.
If the amount of water available for condensation in the cloud is not changed, this means that there will be more smaller drops, which are less likely to grow to sufficient size to fall out as precipitation and making clouds last longer, again contributing to cooling.
For two reasons, therefore, - cooling of the surface because of increased reflection of solar energy, and reduced efficiency of clouds to produce rain ? increases in aerosol will weaken the hydrological cycle.
As far as precipitation goes, contrail cirrus seems to behave in the same manner as natural cirrus (as I suspected). The ice crystals grow to large enough sizes to precipitate. I still don't see why you think contrails can lead to droughts.
Originally posted by luxordelphi
reply to post by Phage
[
There are two methods here - kind of like the changing of the guard. The old one was to increase cirrus coverage. That produced drought conditions.
It also had a net warming effect which became a no no so a new method was put into play. The object of this new method is no clouds at all.
Observationally, the new clouds, the ones with virga, produce, at times some huge, heavy drops - like one or two and then they too are dust in the wind.
But the article you've been talking about says the opposite. It says that aviation increases forcing. That it has warming effect. Not, as you claim, a cooling effect.
2010 Research on Global "sun block" needed now
"Solar-radiation management may be the only human response that can fend off rapid and high-consequence climate change impacts. The risks of not doing research outweigh the risks of doing it," says Keith, director of the Institute for Sustainable Energy, Environment and Economy's energy and environmental systems group and a professor in the Schulich School of Engineering.
Solar-radiation management (SRM) would involve releasing megatonnes of light-scattering aerosol particles in the upper atmosphere to reduce Earth's absorption of solar energy, thereby cooling the planet. Another technique would be to release particles of sea salt to make low-altitude clouds reflect more solar energy back into space.
Field tests of SRM are the only way to identify the best technologies and potential risks, Keith says. He and the American scientists propose carefully controlled testing that would involve releasing tonnes – not megatonnes – of aerosols in the stratosphere and low-altitude clouds.
"If SRM proves to be unworkable or poses unacceptable risks, the sooner we know the less moral hazard it poses; if it is effective, we gain a useful additional tool to limit climate damages.".
www.sciencedaily.com...
Still, it will take decades to develop air capture and algal bioenergy systems, scale up prototypes, prepare underground carbon repositories and deploy such systems on a global scale.
"In an ideal case, we could have full deployment on a global scale by 2050," said Greene.
To buy time, another geoengineering strategy that many scientists are exploring involves altering the Earth's radiation budget by injecting sulfate aerosols into the atmosphere and blocking the sun's rays, mimicking what happens after a volcanic eruption, says the paper. Other strategies involve injecting seawater droplets into clouds and deploying shades or mirrors in space, all to block the sun's rays from reaching Earth's surface.
Such solar radiation management strategies "can be done quickly, but should only be considered as a last resort to buy ourselves some time" since they simply "cover up the problem without doing anything about the CO2," said Greene.
www.sciencedaily.com...
This new study looked at the impacts of different strengths of geoengineering, from full strength (sufficient to return global average temperatures back to normal), through to no geoengineering.
Their analysis revealed that with increasing geoengineering strength, most regions become drier while others buck the trend and become increasingly wet. For example, the USA became drier with increasing geoengineering, and returned to normal conditions under half-strength geoengineering, whereas Australia became wetter, returning to normal conditions only for full strength geoengineering
A factor of 5000 would be rather significant. Do you have a quote for that?
A single aircraft operating in conditions favorable for persistent contrail formation appears to exert a contrail-induced radiative forcing some 5000 times greater (in W m?2km?1) than recent estimates of the average persistent contrail radiative forcing from the entire civil aviation fleet.
Are you actually going anywhere with this, or is mindless repetition of readily available info your only goal??
So what else where the rockets were not too visible?
Originally posted by luxordelphi
SRM: a bloody nightmare.
Originally posted by luxordelphi
reply to post by Aloysius the Gaul
Are you actually going anywhere with this, or is mindless repetition of readily available info your only goal??
You said:
So what else where the rockets were not too visible?
So I told you about what else where the rockets were not too visible because that's the only part of your post that wasn't repetitious. The repetition is eating me alive.
The stratosphere is impacted by jet emissions. The tropopause is impacted by jet emissions. The troposphere is impacted by jet emissions. The hydrological cycle is impacted by jet emissions. Net warming is impacted by jet emissions.
SRM: a bloody nightmare.
Originally posted by luxordelphi
reply to post by Uncinus
A factor of 5000 would be rather significant. Do you have a quote for that?
Here's the quote from this link:
www.ipcc.ch...
A single aircraft operating in conditions favorable for persistent contrail formation appears to exert a contrail-induced radiative forcing some 5000 times greater (in W m?2km?1) than recent estimates of the average persistent contrail radiative forcing from the entire civil aviation fleet.