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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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The April issue of 'Weather' has a fascinating article by W.S. Pike
detailing the history of Biggin Hill meteorological office(s) since 1917. ( For those that don't subscribe, I believe you can get 'one-off' issues from the RMetSoc: see .. http://www.rmets.org/membership/subscriptions.php ) As part of this article, there is a facsimile extract from the Observations Register for August 1940, specifically for the 30th. This is interesting in several ways:- 1. The code form, and the manner of entry of weather types (using Beaufort letters) will be familiar to many who have worked in operational meteorology, and it is interesting to see how things have changed, and how some things have not. The code form itself was in use from well before the Second World War (being listed in my copy of the Admiralty Weather Manual of 1938), and I believe was not superseded until the 'Washington' code was introduced in the late 1940's. One of the differences from format we are now familiar with is the manner of coding wind direction - compass points are used, applying the 32-point scheme; so north = 32, south = 16, east = 08 etc. Also, the lower 'ww' figures are significantly different: 08 = mist (now 10), whereas for the higher numbers (50's upwards) although there are differences, they are not so great. 2. The economy of space is marked. A single page contains all the observations for one day, plus extremes, time-marks, additional information etc. When manuscript entering of observations ended in the Met Office, the DR for one day covered two over-large pages and took up a huge expanse of the observer's table: (accidents with tea cups increased when the code form changed to that now in use!) 3. The day itself was fine; a cold start (grass min 30°F) with a hoar frost recorded in the Beaufort letters between 04 and 07GMT; this would not be unusual for this location at the end of August, being some 600ft asl. Some shallow Cumulus forming between 08 and 15GMT with Cirrus above. The total cloud amounts never more than 3/10's with good visibility (after the morning mist). The synoptic situation could be inferred even without reference to a chart. A gentle northerly wind, sometimes calm, with a NEPH report made at 06GMT showing a Cirrus motion from 330deg, with speed 55mph (circa 48 knots, though such accuracy of conversion wouldn't be justified with the technique). A ridge (surface and upper) lay to the west of the station, but with a weakening gradient flow after quite a strong northerly of the previous day (which presumably brought the chilly, low humidity air across the SE). You can see the situation by looking at the Re-analysis charts on the Wetterzentrale site:- http://www.wetterzentrale.de/topkarten/fsslpeur.html 4. By far the most poignant aspect of this diagram (and the reason why it is in the article) is that on this day, Biggin Hill was attacked (twice), along with many other Fighter Command airfields in the southeast of England .. see:- http://www.raf.mod.uk/bob1940/august30.html There were four observers on this airfield, three of them having entries in the Daily Register for the 30th August, 1940. (They were presumably working an EMN variant). The last hourly observation on this near-perfect day was at 1700GMT; the space for the remaining observations was headed up ready for entry, but the rest of the page is blank. As Pike notes in the article, all three observers were killed whilst taking shelter. The only allusion to this event is the bald statement by the fourth observer: - " Observations abandoned at 1700. Instruments rendered useless as a result of enemy action ". -- FAQ & Glossary for uk.sci.weather at:- http://homepage.ntlworld.com/booty.weather/uswfaqfr.htm |
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