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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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#1
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How common is this?
http://www.metoffice.gov.uk/weather/..._pressure.html 23 November 2011. The High over Greenland. |
#2
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In article
, Weatherlawyer writes: How common is this? http://www.metoffice.gov.uk/weather/..._pressure.html 23 November 2011. The High over Greenland. I had a look, but it's now the chart for the 24th. The "high" is still there, but is now shown as 998mb. I think it's a case of a computer algorithm getting over-enthusiastic, and labelling a very minor and local peak as a "high". The main high pressure centre is well to the west, as shown by the isobars. There's at least one other such pseudo-high shown on the map, over Germany, and a pseudo-low just to the west of Greenland. -- John Hall "The power of accurate observation is commonly called cynicism by those who have not got it." George Bernard Shaw |
#3
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On Nov 24, 10:30*am, John Hall wrote:
In article , *Weatherlawyer writes: How common is this? http://www.metoffice.gov.uk/weather/..._pressure.html 23 November 2011. The High over Greenland. I had a look, but it's now the chart for the 24th. The "high" is still there, but is now shown as 998mb. I think it's a case of a computer algorithm getting over-enthusiastic, and labelling a very minor and local peak as a "high". The main high pressure centre is well to the west, as shown by the isobars. There's at least one other such pseudo-high shown on the map, over Germany, and a pseudo-low just to the west of Greenland. The median point is the 1016 mb line though much less that 8 either side of it counts as col or misty stuff going nowhere. Do you mean those 1025 thingies east of the 1043? The Lows in the Arctic/North Atlantic are residual from the earthquakes and Kenneth that spawned or/and increased during this spell. They should have congealed by now according the the T+12 and are heading this way. Which means another series of quakes starting up somewhere west of Iceland and heading down to Indonesia via Japan. The spell ends tomorrow (the lunar perigee was yesterday, I am still pondering what happened with that.) Take a look at Bernard Burton's site for the ASSX charts, don't be misled by Google searching for brothels for you there though. Perhaps he aught to change the title of that link. OTOH he will get more hits with a sexy title. I've posted some of the stuff I found, you know where -seek and ye shall find. |
#4
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Highs and lows are only defined relative to surrounding pressure and
are a human construct. There are no absolutes. The notation in this instance merely marks the point of highest pressure in that locale. Plus, yes, enthusiastic labelling. Stephen. |
#5
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On Nov 24, 1:04*pm, Stephen Davenport wrote:
Highs and lows are only defined relative to surrounding pressure and are a human construct. There are no absolutes. The notation in this instance merely marks the point of highest pressure in that locale. Plus, yes, enthusiastic labelling. Or maybe they were looking ahead? A new spell starts tomorrow but look at T+24 anyway. 06:11 means fog with no Greenland High, not sure about the European one though. The charts does not give the impression its constructors were certain of themselves. And I've been waiting for a largish shoe to drop. Can't think why though. Just a gut feeling. Ah, there we go, news just in: 6.2 2011/11/24 10:25:35 41.877 142.710 42.3 HOKKAIDO, JAPAN REGION Hmmm... Maybe it has to go down before it turns up? |
#6
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On Nov 24, 1:04*pm, Stephen Davenport wrote:
Highs and lows are only defined relative to surrounding pressure and are a human construct. There are no absolutes. The notation in this instance merely marks the point of highest pressure in that locale. Plus, yes, enthusiastic labelling. Stephen. I would guess though that (at least in the N Hemisphere winter) that lower central pressure "highs" are more likely further north over Greenland/Iceland/Norway given the low mean surface pressure in this region? ( e.g. http://badc.nerc.ac.uk/data/ecmwf-era/pics/mslp.gif ) Richard |
#7
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On Nov 24, 1:53*pm, Richard Dixon wrote:
On Nov 24, 1:04*pm, Stephen Davenport wrote: Highs and lows are only defined relative to surrounding pressure and are a human construct. There are no absolutes. The notation in this instance merely marks the point of highest pressure in that locale. Plus, yes, enthusiastic labelling. Stephen. I would guess though that (at least in the N Hemisphere winter) that lower central pressure "highs" are more likely further north over Greenland/Iceland/Norway given the low mean surface pressure in this region? ( e.g.http://badc.nerc.ac.uk/data/ecmwf-era/pics/mslp.gif) Richard The High is not real anyway because MSL pressures over the Greenland icecap are meaningless. The place only has "mean sea level" at the edges and the interior is far too high for any extrapolation to sea level to be useful. It's probably best to regard Greenland as a discontinuity in the MSL pattern and to regard the isobars as formalities which do not necessarily bear any relation to the circulation at the land surface. The same is true of Antarctica, even more so because of the greater extent and altitude of the continent. Tudor Hughes, Warlingham, Surrey. |
#8
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Tudor Hughes wrote:
On Nov 24, 1:53 pm, Richard Dixon wrote: On Nov 24, 1:04 pm, Stephen Davenport wrote: Highs and lows are only defined relative to surrounding pressure and are a human construct. There are no absolutes. The notation in this instance merely marks the point of highest pressure in that locale. Plus, yes, enthusiastic labelling. Stephen. I would guess though that (at least in the N Hemisphere winter) that lower central pressure "highs" are more likely further north over Greenland/Iceland/Norway given the low mean surface pressure in this region? ( e.g.http://badc.nerc.ac.uk/data/ecmwf-era/pics/mslp.gif) Richard The High is not real anyway because MSL pressures over the Greenland icecap are meaningless. The place only has "mean sea level" at the edges and the interior is far too high for any extrapolation to sea level to be useful. It's probably best to regard Greenland as a discontinuity in the MSL pattern and to regard the isobars as formalities which do not necessarily bear any relation to the circulation at the land surface. The same is true of Antarctica, even more so because of the greater extent and altitude of the continent. Are isobars over other extensive highland areas such as the Tibetan plateau regarded in the same fashion? -- Col Bolton, Lancashire 160m asl |
#9
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![]() "Col" wrote in message ... Tudor Hughes wrote: On Nov 24, 1:53 pm, Richard Dixon wrote: On Nov 24, 1:04 pm, Stephen Davenport wrote: The High is not real anyway because MSL pressures over the Greenland icecap are meaningless. The place only has "mean sea level" at the edges and the interior is far too high for any extrapolation to sea level to be useful. It's probably best to regard Greenland as a discontinuity in the MSL pattern and to regard the isobars as formalities which do not necessarily bear any relation to the circulation at the land surface. The same is true of Antarctica, even more so because of the greater extent and altitude of the continent. Are isobars over other extensive highland areas such as the Tibetan plateau regarded in the same fashion? -- Col Bolton, Lancashire 160m asl Yes - a bit like thickness charts. There's so much interpolation down to sea level that they are pretty much worthless. -- Freddie Bayston Hill Shropshire 102m AMSL http://www.hosiene.co.uk/weather/cumulus/ |
#10
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On Nov 24, 7:02*pm, "Col" wrote:
Tudor Hughes wrote: On Nov 24, 1:53 pm, Richard Dixon wrote: On Nov 24, 1:04 pm, Stephen Davenport wrote: Highs and lows are only defined relative to surrounding pressure and are a human construct. There are no absolutes. The notation in this instance merely marks the point of highest pressure in that locale. Plus, yes, enthusiastic labelling. Stephen. I would guess though that (at least in the N Hemisphere winter) that lower central pressure "highs" are more likely further north over Greenland/Iceland/Norway given the low mean surface pressure in this region? ( e.g.http://badc.nerc.ac.uk/data/ecmwf-era/pics/mslp.gif) Richard * * * * * * * The High is not real anyway because MSL pressures over the Greenland icecap are meaningless. *The place only has "mean sea level" at the edges and the interior is far too high for any extrapolation to sea level to be useful. *It's probably best to regard Greenland as a discontinuity in the MSL pattern and to regard the isobars as formalities which do not necessarily bear any relation to the circulation at the land surface. *The same is true of Antarctica, even more so because of the greater extent and altitude of the continent. Are isobars over other extensive highland areas such as the Tibetan plateau regarded in the same fashion? -- Col Bolton, Lancashire 160m asl- Hide quoted text - - Show quoted text - In South Africa, AFAIK, the standard method is to use the 850 mb height (in effect the pressure at about 5000 ft) as the surface isobars. This wouldn't work for Cape Town or Durban, for example and the MSL isobars are then used, there being a discontinuity on the charts. This is not as bad as it might seem since the drop from the tableland to sea level is fairly abrupt. As Freddie mentions, all this has an effect on 1000-500 thickness values and an interesting example is seen in comparing Ojmjakon with Jakutsk in winter. Both are extremely cold (-45 and -50 routinely) and lie under spectacular inversions of 20 deg and more. Since Ojmjakon is so much higher than Jakutsk (740 m vs 100 m) the surface temperature at Ojmjakon is much lower than that in the free air at the same height over Jakutsk and this low figure is extrapolated to sea level thus in effect creating a virtual inversion 700 m deep and at -50°C. There is simply no way of getting a meaningful 1000-500 mb thickness from Ojmjakon under these conditions. The high altitude of the surface simply pushes the whole inversion upwards. In summer (briefly) the opposite applies, Ojmjakon being a high-level heat source like the Tibetan plateau and many other areas. Tudor Hughes, Warlingham, Surrey. |
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