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uk.sci.weather (UK Weather) (uk.sci.weather) For the discussion of daily weather events, chiefly affecting the UK and adjacent parts of Europe, both past and predicted. The discussion is open to all, but contributions on a practical scientific level are encouraged. |
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I can understand why low pressure cells are deeper in winter - greater
temperature contrast, but what mechanism causes winter high pressure cells to have higher central values than summer ones? -- Paul Hyett, Cheltenham (change 'invalid83261' to 'blueyonder' to email me) |
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On Dec 13, 8:59�am, Paul Hyett wrote:
I can understand why low pressure cells are deeper in winter - greater temperature contrast, but what mechanism causes winter high pressure cells to have higher central values than summer ones? -- Paul Hyett, Cheltenham (change 'invalid83261' to 'blueyonder' to email me) Its partly a case of what goes up must come down. The large amount of rising air needed for a deep low descends somewhere to form an intense high. Also the intense radiational cooling over the continents in winter adds to the effect through the extra density of the cold boundary layer air. Dick Lovett Charlbury |
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On Dec 13, 8:59 am, Paul Hyett wrote:
I can understand why low pressure cells are deeper in winter - greater temperature contrast, but what mechanism causes winter high pressure cells to have higher central values than summer ones? Short answer is that cold air is denser. So total column density is larger. Clear skies of a high with limited hours of winter insolation tend to allow the nights to be colder and self reinforcing. The sun is very low in the sky this time of year. It is a very cold frosty day with bright azure blue sky and golden sunshine up here in N Yorks today. Regards, Martin Brown |
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On Dec 13, 9:52 am, Dick Lovett wrote:
On Dec 13, 8:59�am, Paul Hyett wrote: I can understand why low pressure cells are deeper in winter - greater temperature contrast, but what mechanism causes winter high pressure cells to have higher central values than summer ones? -- Paul Hyett, Cheltenham (change 'invalid83261' to 'blueyonder' to email me) Its partly a case of what goes up must come down. The large amount of rising air needed for a deep low descends somewhere to form an intense high. Also the intense radiational cooling over the continents in winter adds to the effect through the extra density of the cold boundary layer air. Sort of knock the theory about low pressure raising so many inches of North Sea into a cocked hat doesn't it? All it's got to do is cool down to affect all that hot air. So why doesn't it strap all that high pressure instead of raising a tide? Does it even suck in the right direction? |
#5
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On Dec 13, 8:59 am, Paul Hyett wrote:
I can understand why low pressure cells are deeper in winter - greater temperature contrast So what causes greater temperature differences? |
#6
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In article
, Weatherlawyer writes: On Dec 13, 8:59 am, Paul Hyett wrote: I can understand why low pressure cells are deeper in winter - greater temperature contrast So what causes greater temperature differences? The temperature at the Equator doesn't change much throughout the year, as the sun at local noon is always within 23 degrees or so of the vertical, and the length of time between sunrise and sunset doesn't change much either. But close to the Pole you have almost six months with no sun, so naturally there is a large difference in temperature between winter and summer. That produces a much greater temperature difference between Polar and Equatorial regions in winter than in summer. -- John Hall "Honest criticism is hard to take, particularly from a relative, a friend, an acquaintance, or a stranger." Franklin P Jones |
#7
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In uk.sci.weather on Thu, 13 Dec 2007, Dick Lovett
wrote : On Dec 13, 8:590 I can understand why low pressure cells are deeper in winter - greater temperature contrast, but what mechanism causes winter high pressure cells to have higher central values than summer ones? -- Paul Hyett, Cheltenham (change 'invalid83261' to 'blueyonder' to email me) Its partly a case of what goes up must come down. The large amount of rising air needed for a deep low descends somewhere to form an intense high. Also the intense radiational cooling over the continents in winter adds to the effect through the extra density of the cold boundary layer air. OK, that makes sense. -- Paul Hyett, Cheltenham (change 'invalid83261' to 'blueyonder' to email me) |
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