hallmark007
Captain
Flight distance : 9827923 ft
Ireland
Offline
|
gyrex Posted at 2018-10-27 23:35
His post, for the most part, is all word salad and makes no sense, whatsoever. For a start, the troposphere starts from around 6-10km above sea level. Wind can increase in speed as it funnels through valleys but it's hard to estimate whether or not this is the case in this example. A more concerning phenomenon around mountains is katabatic winds where, as warm air rises up one side of a mountain, the air is suddenly cooled as it travels up the mountain and then the cool air rushes down the other side of the mountain at incredible speeds - sailors are well aware of this - especially in the afternoons. I've seen, first hand the immense effects of katabatic winds whilst sailing in Greece and Croatia.
First up it was meant as a joke from a conversation between JJB , your good friend jumped in as he has some sort of fetish trolling me, something I know plenty about is weather and mountains and there was nothing wrong in what I said, I did not apply it to the op’s Case as you will have read my earlier post, or did you.
Wind, Rain and Snow
Warm air is lighter than cold air, so the air at ground level tends to rise, displacing the cold air at higher elevations, which falls. This creates convection currents throughout the troposphere, and they are more predominant at higher elevations, where the air is less dense and can move more freely. Consequently, winds are stronger at higher elevations. Colder temperatures at higher elevations also create precipitation, because cold air can't hold as much moisture as warm air. Moisture condenses out of the air as snow and ice, and it falls back to the ground. At lower elevations, where the temperature is warm, it turns to rain, but that doesn't happen at higher elevations where the temperature hasn't risen above freezing. |
|