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Originally posted by ThirdRock69
I did read that above the tropopause the air can increase in temp.
So if a plane were flying in the lower colder region of the tropopause and another plane was flying in the higher warmer region of the stratosphere.
It is possible for the higher plane to make a less persistent contrail.
Originally posted by ThirdRock69
reply to post by AwakeinNM
Originally posted by ThirdRock
The higher you go the colder it gets, the less pressure and humidity. Yes there are small variances but not enough to cause the degree of difference in the two types of contrails.
I already posted this. At least comment on the video. Which "contrail" appears to be at a higher altitude in the video?
Originally posted by JAsay1LOVE
reply to post by Uncinus
thank you for further clarification. i would ask though, you said at 90000 ft "essentially" no planes fly there. I am a novice in aerospace information, so do some planes, and can planes fly at that altitude? not asking in a manner to lead to they are up there all the time, but simply, do and could some planes fly at said height; and if so, could they produce the occurring thirdrock69 is attempting to portray?
Originally posted by JAsay1LOVE
but could anyone offer an explanation for how in the same day that in the morning is completely clear- in a matter of just a couple hours there are upwards of 25 lines in a checkerboard pattern.
2.1. Potential seeding material
An ideal ice nucleating agent for cirrus geoengineering would be one having a high effectivity (for ice nucleation) at temperatures colder than ~ –20 °C, but a very low effectivity at warmer temperatures. Bismuth tri-iodide (BiI3) had been investigated as an ice nucleant for weather modification programs but was unsuitable because its effectivity threshold was below –10 °C. However, this makes it a suitable ice nucleant for geoengineering, targeting primarily cirrus clouds and not the clouds normally targeted in cloud seeding experiments. In addition, BiI3 is non-toxic and reagent grade bismuth metal is about 1/12th the cost of silver, suggesting BiI3 would be about 1/12th the cost of AgI.
Bismuth tri-iodide can be generated in aerosol form by combustion of an alcohol solution of BiI3 (solubility, 3.5 g/100 ml). A better aerosol generating system for this nucleant is pyrotechnic combustion. For this, a modest program of research and development would be required. A pressed composite mixture of BiI3, potassium perchlorate (KClO4), aluminum and gilsonite (a natural hydrocarbon) would be appropriate.
2.2. Delivery mechanism
Since commercial airliners routinely fly in the region where cold cirrus clouds exist, it is hoped that the seeding material could either be (1) dissolved or suspended in their jet fuel and later burned with the fuel to create seeding aerosol, or (2) injected into the hot engine exhaust, which should vaporize the seeding material, allowing it to condense as aerosol in the jet contrail. The objective would not be to seed specific cloud systems but rather to build up a background concentration of aerosol seeding material so that the air masses that cirrus will form in will contain the appropriate amount of seeding material to produce larger ice crystals. Since the residence time of seeding material might be on the order of 1–2 weeks, release rates of seeding material would need to account for this. With the delivery process already existing, this geoengineering approach may be less expensive than other proposed approaches.
2.3. Production of new cirrus
Aircraft (Helten et al 1998, Spichtinger et al 2004) and microwave limb sounder (MLS) satellite measurements (Read et al 2001, Spichtinger et al 2003) show that large portions of the clear-sky upper troposphere are supersaturated with respect to ice. While natural cirrus may or may not form in these regions over time, the global, quasi-uniform distribution and continuous introduction of efficient heterogeneous ice nuclei might produce more cirrus clouds in these regions than would otherwise occur. Over time, the relatively large ice crystals would sediment to lower levels and warmer temperatures where the cirrus greenhouse effect is less. Water vapor concentrations in the upper troposphere should decrease with this export of moisture to lower levels, and the water vapor greenhouse effect in the upper troposphere should decrease. In fact, the upper troposphere water vapor content in GCMs (affecting the clear-sky OLR) is sometimes `tuned' by changing the ice fall speed.
are there this many flights in such a small window?
Originally posted by Phage
reply to post by JAsay1LOVE
are there this many flights in such a small window?
You can get near realtime information here:
flightaware.com...
Select an airport in your vicinity (in the right side panel) and click "view activity". It can help to zoom the view out a bit.
edit on 2/29/2012 by Phage because: (no reason given)
i completely understand that. semi expected that. but even if its a 30 min lag, it would still show the 6 planes moving in cris-cross patterns would it not?
what about the reverse? i.e. i see the multiple planes then i go to the website and check to see if those many planes are recorded. follow me?