Rich West
EF0
- Joined
- Feb 9, 2012
- Messages
- 27
Hi all
It was suggested that my original question might be being missed, due to the thread title, so I have reposted here.
The link to the discussion so far is:
http://www.stormtrack.org/forum/showthread.php?28649-Greetings-and-Introductory-Post
When I got into meteorology last year it seemed straightforward that high pressure areas involved sinking air. Then I saw a sky, under the high pressure system we had at the time, filled to the horizon with Stratocumulus. If the air is subsiding I wanted to know how clouds were forming as this required lift or stationary air at the least. At another time I noticed frontal systems spreading through the high pressure systems on the MET surface charts. I wanted to know how these "low pressure system phenomena" were spreading deep into (and sometimes through) the high.
Odd patches of cloud (like the other day's alto cumulus) seem to be small features and are probably related to orographic lifting. However, the Sc, being 8/8 at points, seems to be a different phenomena in my newbie eyes. I eventually found (after a huge amount of search time) a diagram (without detail) that showed HP sometimes subsiding from below cirrus level to just above Sc level (where it diverges/diffluences(?)). This made sense of the clouds' existences. However, if the air was outwardly horizontal above Sc level then why the hell was the ground showing a high barometric reading? This was my initial question that was never cleared up.
My own stab at a hypothesis after thinking I might never get to the bottom of this was:
"The air below Cirrus and above Stratocumulus is descending as it should. The air from ground up to the top of Sc is stationary, however, I think the subsiding atmosphere might be compressing the stationary layer and thus causing it to be high pressure too. Obviously I can't say for sure as the experts are silent but that's my newbie guess."
Any data on this general question or the frontal impingements woudl be gratefully received.
Cheers
Rich
It was suggested that my original question might be being missed, due to the thread title, so I have reposted here.
The link to the discussion so far is:
http://www.stormtrack.org/forum/showthread.php?28649-Greetings-and-Introductory-Post
When I got into meteorology last year it seemed straightforward that high pressure areas involved sinking air. Then I saw a sky, under the high pressure system we had at the time, filled to the horizon with Stratocumulus. If the air is subsiding I wanted to know how clouds were forming as this required lift or stationary air at the least. At another time I noticed frontal systems spreading through the high pressure systems on the MET surface charts. I wanted to know how these "low pressure system phenomena" were spreading deep into (and sometimes through) the high.
Odd patches of cloud (like the other day's alto cumulus) seem to be small features and are probably related to orographic lifting. However, the Sc, being 8/8 at points, seems to be a different phenomena in my newbie eyes. I eventually found (after a huge amount of search time) a diagram (without detail) that showed HP sometimes subsiding from below cirrus level to just above Sc level (where it diverges/diffluences(?)). This made sense of the clouds' existences. However, if the air was outwardly horizontal above Sc level then why the hell was the ground showing a high barometric reading? This was my initial question that was never cleared up.
My own stab at a hypothesis after thinking I might never get to the bottom of this was:
"The air below Cirrus and above Stratocumulus is descending as it should. The air from ground up to the top of Sc is stationary, however, I think the subsiding atmosphere might be compressing the stationary layer and thus causing it to be high pressure too. Obviously I can't say for sure as the experts are silent but that's my newbie guess."
Any data on this general question or the frontal impingements woudl be gratefully received.
Cheers
Rich