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Originally posted by OzWeatherman
I dont want youtbe videos as evidence, they arent reliable enough.
Originally posted by cutbothways
reply to post by OzWeatherman
Again, you are wrong.
Contrails form by water vapor clinging to the dust in the exhaust.
So, the air need to be at least -40c or less, 250mb or more, and "quite humid" according to NASA, the Appleman Chart, and you.
Now, read this.
At usual airline cruise altitudes of 9,144 to 11,877 m (30,000-39,000 ft),
the ambient air has little humidity.
Source
Note: Although not restricted, the cargo compartments on our Airbus A319, A320, and A321 aircraft are not heated and temperatures can be as low as two degrees Celsius, so it is not recommended to transport animals on these aircraft during the winter season.
www.aircanada.com...
As low as 2C in the winter? I thought -40C happened all the time. How do you explain this?
Originally posted by dAlen
Its easy to throw out titles, "Im a meteorologist", or "airplane pilot".
There is not even a consensus among them about topics such as this.
You can look at our own board to see that this would appear to be the case.
[edit on 7-5-2008 by dAlen]
And the inside temperature of an aircraft has no relevance on the temperature outside of the air craft. Thats just common sense
Originally posted by OzWeatherman
But I genuinely am.
I have proof, just email my work address (which I am happy to U2U to anyone who wants it) and I will email you back
Originally posted by cutbothways
reply to post by OzWeatherman
So, what are the atmospheric conditions required for a contrail to form.
By the way, if the ambient temperature on the exterior of the aircraft is -40, and the interior that is not heated stays at a comfy 2C, and it only gets this cold in the winter time, doesn't that suggest -40C even at 30000 ft is rare?
8328 -41.9 -58.5 15
RH (percent)
hpa . 0 30 60 90 100
30.0 -69.61 -68.67 -67.36 -64.93 -61.74
50.0 -65.53 -64.54 -63.17 -60.64 -57.15
100.0 -59.68 -58.63 -57.17 -54.47 -50.92
115.0 -58.45 -57.39 -55.91 -53.17 -49.61
130.0 -57.36 -56.29 -54.79 -52.02 -48.43
150.0 -56.07 -54.99 -53.47 -50.66 -47.01
175.0 -54.67 -53.56 -52.02 -49.18 -45.42
200.0 -53.43 -52.31 -50.76 -47.87 -44.12
250.0 -51.33 -50.19 -48.60 -45.65 -41.80
300.0 -49.58 -48.42 -46.80 -43.79 -39.87
350.0 -48.07 -46.89 -45.25 -42.20 -38.23
400.0 -46.75 -45.55 -43.89 -40.80 -36.77
450.0 -45.57 -44.36 -42.67 -39.54 -35.46
500.0 -44.50 -43.27 -41.57 -38.41 -34.28
600.0 -42.62 -41.37 -39.63 -36.41 -32.18
700.0 -41.00 -39.73 -37.97 -34.69 -30.40
800.0 -39.58 -38.29 -36.50 -33.18 -28.84
900.0 -38.30 -37.00 -35.19 -31.82 -27.43
1000.0 -37.15 -35.84 -34.00 -30.60 -26.15
Fig. 4. RHI (%) at 225 hPa from RUC-2 analyses, 9-12-2001.
Over PA, RHI ranges from 90% at the OH border to
50% at the eastern PA border. Over Pittsburgh (PIT)
underneath contrail A at 1200 UTC, the RUC RHI is
80%, while near Aberdeen, MD (ABD), close to C at
1200 UTC, RHI = 55%. A similar value is found over
Dulles, VA (IAD) near contrail D, while RHI = 80% over
Blacksburg, VA (BLK) near the end of E. These values
are too low for sustaining contrails. To determine if
these values are due to the model assimilation process,
the rawinsonde RHI profiles are compared with the
corresponding RUC values at 1200 UTC. in Fig. 5. The
RUC increased RHI at most levels over BLK and PIT
while smoothing or decreasing RHI over ABD and IAD.
No contrails were observed for RHI < 55%
Like natural cirrus clouds, contrails can impact
climate through their radiative effects. Persistent
contrails often form in air with relative humidities with
respect to ice (RHI) exceeding 100% but with relative
humidities with respect to water (RH) less than 100%.
Originally posted by SantaClaus
Starred neformore, I love those pictures of pre-50's contrails. I mean, that should end this conspiracy flat out, no?
Originally posted by cutbothways
Why can't you guys address the problem with humidity.
Need to be near 100% humidity for a contrail to form
normally.
Fig. 4. RHI (%) at 225 hPa from RUC-2 analyses, 9-12-2001.
Over PA, RHI ranges from 90% at the OH border to
50% at the eastern PA border. Over Pittsburgh (PIT)
underneath contrail A at 1200 UTC, the RUC RHI is
80%, while near Aberdeen, MD (ABD), close to C at
1200 UTC, RHI = 55%. A similar value is found over
Dulles, VA (IAD) near contrail D, while RHI = 80% over
Blacksburg, VA (BLK) near the end of E. These values
are too low for sustaining contrails. To determine if
these values are due to the model assimilation process,
the rawinsonde RHI profiles are compared with the
corresponding RUC values at 1200 UTC. in Fig. 5. The
RUC increased RHI at most levels over BLK and PIT
while smoothing or decreasing RHI over ABD and IAD.
No contrails were observed for RHI < 55%
www-pm.larc.nasa.gov...
Again, I have exposed your BS.
According to the above NASA pdf,
even a 90% relative humidity (with respect to ice) was too low to sustain contrails.
And zero contrails were observed below 55% RHi.
Like natural cirrus clouds, contrails can impact
climate through their radiative effects. Persistent
contrails often form in air with relative humidities with
respect to ice (RHI) exceeding 100% but with relative
humidities with respect to water (RH) less than 100%.
Originally posted by OzWeatherman
Ok, this is probably my last reply on this thread as the Op appears to be lying about being a pilot and cant seem to read
Never said I was a pilot. I flew as crew chief (engineer) on the P-3
All the other is classified. But I flew many times before the Navy. My
father was Swedish. I've made the trip to Sweden a few times.
The Op is suggesting ridiculous theories like temperature inside the aircraft is the same as the outside ambient temperature of the upper atmosphere
If you look up on a sunny day and see in the cloudless sky a jet leaving a long, white plume, then rain, snow or some other form of precipitation may be on the way. That white plume is called a contrail. It is the condensation trail of ice crystals left behind by the exhaust of a flying jet aircraft. These aircraft fly 8 to 12 kilometres above the ground pulling in very cold, dry air and spewing out hot, water-filled exhaust. The hot water vapour mixes with the colder surrounding air, and in the process, expands and then freezes in 1 or 2 seconds forming a trail of ice crystals.
If a jet leaves no trail or only a short trail or if the trail fades quickly then the air at that level is relatively dry. This means the fair weather is likely to continue. But, if the exhaust trail lingers for an hour or more or spreads across the sky, that means the surrounding air is moist and rain or some other form of precipitation may be on the way.
I agree, even if the baggage or gear part of the aircraft isn't heated, wouldn't the heat from the cabin portion of the plane warm it up even if just a little bit? theres no way it could be -40 inside the plane anywhere. Even if it was in an area where there were no pets IE: not heated, things like gel, shampoo, etc or any other liquid would freeze solid
Furthermore, the luggage is typically stored in areas of the plane which are subject to the variations of temperature and pressure which occur as a function of altitude. Specifically, the temperature and pressure within the baggage compartment will decrease substantially as the airplane reaches cruising altitude, often times subjecting the luggage contents to temperatures below their particular freezing points.