![]() |
If this is your first visit, be sure to check out the FAQ by clicking the link above. You may have to register before you can post: click the register link above to proceed. To start viewing messages, select the forum that you want to visit from the selection below. |
|
|
Thread Tools | Display Modes |
#27
|
|||
|
|||
![]()
On Feb 10, 9:47 am, Mxsmanic wrote:
So, overall, the air is always warmest at the surface. There are some anomalies higher in the atmosphere. Not always. Not at all always. We frequently get inversions where the air 1000' feet up is much warmer than that on the surface. Inversions are very common here, and I would imagine they're common most anywhere away from the equator. We've had days here, in the winter, where we've left the ground where the temp is -20°C, and found -18°C at 3000' agl. Often I find the winds howling at 25 or 30 knots just 200 feet above the surface, while the wind on the ground is zilch and the temp is 25 degrees colder. "Always" just doesn't deal with reality. Works on a sim, I suppose. Parcels of air that rise in the atmosphere will cool as the pressure in the atmosphere drops, and this is responsible the adiabatic lapse rate. If you'd ever studied meteorology (Commercial Pilot groundschool) you'd know that the temp falls with altitude until we reach the tropopause. Then it starts rising until we reach the stratopause, where it starts to fall again through the mesosphere, and once we reach the thermosphere it rises again and keeps on rising, though the density is so low that the actual heat content is minimal. See this: http://www.ux1.eiu.edu/~cfjps/1400/FIG01_019.JPG In both cases, the correlation is between temperature and altitude, not temperature and pressure. If pressure rises, so does temperature. The air coming down off the Rockies here rises in temperature as its pressure rises in the descent. This is part of the chinook phenomenon's equation. The rest of that equation has to do with condensation of the vapor on the west side of the mountains, which releases the heat of evaporation back to the atmosphere so that the air's temperature fall is minimal as the air is forced upward by the terrain. So when it gets to 3000' on this side, it's MUCH warmer and drier than it was at 3000' on the west side. The snow evaporates (sublimates) in that warm, dry air. It doesn't have a chance to melt. The atmosphere is much more complex than you think. Dan |
Thread Tools | |
Display Modes | |
|
|
![]() |
||||
Thread | Thread Starter | Forum | Replies | Last Post |
yrb-49-taxi.jpg | [email protected] | Aviation Photos | 2 | September 25th 07 09:50 PM |
Hanoi Taxi | john smith | Piloting | 0 | April 27th 06 03:48 AM |
License To Taxi? | SteveT | Piloting | 29 | October 16th 05 04:57 PM |
Leaning for taxi | Jim Rosinski | Piloting | 28 | September 12th 04 03:53 AM |
taxi in reverse? | [email protected] | Owning | 20 | February 21st 04 12:26 AM |