what is the final temperature of an air parcel moved adiabatically from 10km to 5km?
358112
about 50 degrees celsius less (about -10 degrees celsius for every kilometer increase in altitude), that is assuming the air parcel is unsaturated.
834408
dry adiabatic process
229403
The heat from the explosion carried moist air very quickly to an altitude over 80,000ft.the temp drops 3 degrees every 1000ft.do the math.
769934
It's the actual temperature with humidity, wind chill factor (if applicable), dew point and other conditions taken into consideration. There's actually a mathematical equation to figure it out but it may be hard to find since the calculations are done by computers these days.
216745
One unit kelvin, or 5/9 degree farenheit
791970
Use the Gay-Lussac gas law: V/T is constant. Note that T here is the temperature in Kelvin, not in Celsius. Luckily 27 C = 300 K
274160
32 degrees F\nor \n0 degrees C
200570
the velocity of the ambient
115564
the temperature ranges from aprox. 50 kelvin to 53 kelvin.\nThat on the centigrate scale is -223 C to -220 C.
851569
final speed=initial speed+(acceleration*time)\n=10+(30*30/60)\n=10+15\n=25km/h\nhope that helps..\ngood luck
554161
As answer 4 implies, it defies simple description and modeling, since the lapse rate (rate of change of temperature with altitude) depends on air humidity, and of course that can vary. Up to about 11 KM altitude you can approximate the lapse rate as 6.5 C per km (ref. 1), but that applies to an "international standard atmosphere" which may not exist in your application.\nLooking at the diagrams at the bottom of the page in ref. 2, you can see how a typical real-world weather situation (warm water-laden air blowing onto the shore and passing over a mountain) has a more complex temperature profile.
602468
Absolute Zero or around 20 K.\n\nMelting point 14.01 K  (−259.14 °C, −434.45 °F) \nBoiling point 20.28 K  (−252.87 °C, −423.17 °F)
958888
Use the formula:\nQ (heat) = Cp (Heat Capacity) * delta T (Change in Temperature)
800910
Typically between -20 and +10 degrees Celcius (-4 to +50 F). It depends very much on the amount of humidity in the air. If it is very humid you will start see it at higher temperatures than usual. That's because the air can only contain a certain amount of water vapour at a certain temperature and when the amount of water vapour increases that value the water will condense into liquid water and that's what you see when you "see you breath". The temperature you are referring to is called the dew point and can be found in advanced weather forecasts.
562439
Sin's answer makes sense, but in terms of the environment I'd have thought it would be the highest temperature which combined with wind chill would take the felt temperature down to 0C/32F. But don't trust me - I'm not a scientist.
30743
wood 212° F-450 F\nhay 190F\nCarboard 450F\nPaper bag  451F
210118
Hot and cold air converging over an area of low presure.