How humid can it get in Britain?
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#23
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The really hot air on this day across the southeast was very dry, with dewpoints in single figures, and winds from the southeast.
To the northwest from this hot, dry airmass, there was a band of much higher humidities accompanied by northwesterly winds. It will be through this zone here that you may find an answer. The northwestern boundary of this humid air was accomapnied by severe thunderstorms, one of these allegedly giving nearly 50mm of rain in 10 minutes at Carlton in Cleveland.
N.
#24
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During the mega-downpour days of the mid to late 60's dewpoints of 20 degrees or more were occasionally recorded. 1st July 1968 saw 20+ dewpoints across much of England and Wales before the severe thunderstorms kicked in, and I believe dew-points were almost as high in the warm sector that brought in excess of 100mm of rain from northeast Devon to Lincolnshire during the 10th-11th July of the same year.
N.
#25
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Very high dewpoints were widely recorded across parts of Cent S England, E Wales, N England and the Midlands on the 19th June 2005 prior to the onset of the widespread storm outbreak over the N Midlands and N England during the afternoon. I recall mid-late morning obs with dewpoints of 21 or even 22C from Bham airport, as temps climbed into the mid-high 20s. The moist, low level airmass which may have had its origins from the S and W of Biscay and the W of Portugal was capped off by a dry layer at 850 hPa from the Spanish Plateau. In fact the cap held all day in the S and E Midlands and the S making it feel very opressive (even though dewpoints did fall back to 17-19C).
http://meteocentre.com/archive/analyse/2005/06/19/2005061912_eur.gif
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#29
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Lian,
Humidity can be 100% at any temperature, this when the dew-point of the air is the same as the actual air temp. Normally in this situation you would get fog, water fog if air temp is above freezing and ice or freezing fog if below.
One cannot predict rainfall on humidity alone, though high temperatures and high humidity combined do give conditions for torrential rain, hense why tropical thunderstorms produce so much rain. One also has to consider the interaction of different air-masses, the effect of high pressure and low pressure, of convergence in the lower atmosphere, divergence above, and the effect of jet-streams.
Your 100% humidity was caused by persitent torrential rain lowering the air temp to its dew-point! Hope this all makes sense.
N.
#31
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#32
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Lian - what Nigel is referring to is "relative humidity", a measure of how saturated the air is. 100% means fuly saturated, and the air can absorb no more water vapour.
And indeed rainfall doesn't necessarily mean the air at ground level is fully saturated, nor does reaching 100% relative humidity necessarily mean it's going to start raining (but water vapour might condense out in the form of fog or frost) [he says hoping he's right...]
#33
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I think July (not August) 1995 would have had some high dewpoints. I can remember a day when despite being cloudy overcast and with a strong wind, the shade temperature (admittedly as indicated by a non-standard thermometer and exposure) was above 80 deg. F. (c. 26.7 deg. C.) at my place of work near Portadown, Co. Armagh. The highest for July 1995 (a sunny scorching day) at this site was 29.7 deg. C. on 31st, although 29th June (32.0) and 20th August (31.5 deg. C.) were higher. The official highest temperature in Northern Ireland in 1995 was 30.6 deg. C. at Ballylisk, Co. Armagh, on 2nd August (also NI's highest official August temperature and within 0.2 deg. C. of the overall record for any month).
#34
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Lian,
Humidity can be 100% at any temperature, this when the dew-point of the air is the same as the actual air temp. Normally in this situation you would get fog, water fog if air temp is above freezing and ice or freezing fog if below.
One cannot predict rainfall on humidity alone, though high temperatures and high humidity combined do give conditions for torrential rain, hense why tropical thunderstorms produce so much rain. One also has to consider the interaction of different air-masses, the effect of high pressure and low pressure, of convergence in the lower atmosphere, divergence above, and the effect of jet-streams.
Your 100% humidity was caused by persitent torrential rain lowering the air temp to its dew-point! Hope this all makes sense.
N.
Many thanks for that Nigel, I was about to ask the same or similar question, ie my station has often told me that the humidity was around 98% but the air didnt feel sticky/humid.
And then when watching the weather forecast I would often hear them telling us that it would be a sticky day with humidity up to around 80%, now obviously they are not talking about what I am recording as humidity but they are talking about dew point? Am I right in that presumption? Generally the higher the dew point the more humid it feels and also the more probabilty of some storm activity/lightening? So why record humidity on my station if it isnt really what we all mean as humidity? I think I am loosing myself here....
I know its a basic question, but I am a basic person....thanks!
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#39
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It works fine for me Mungo, here's some of the table for 14:00 BST.
Rhyl (76 m) 19.2° Church Lawford (106 m) 19.0° Kenley (170 m) 18.3° Machrihanish (10 m) 17.0° Charterhall (111 m) 16.6° Ballypatrick Fst (156 m) 16.3° Castlederg (50 m) 16.3° Trawscoed (62 m) 16.0° Ballykelly (5 m) 16.0° Portglenone (65 m) 16.0° Belfast/Aldergrove Airport (68 m) 15.9° Glenanne (160 m) 15.8° Bingley (267 m) 15.8° St Angelo (47 m) 15.7° Holbeach (2 m) 15.6° Glasgow Bishopton (59 m) 15.6° Topcliffe (28 m) 15.5° Loftus Samos (159 m) 15.5° West Freugh (10 m) 15.5° Hereford/Credenhill (76 m) 15.4° Leeming (32 m) 15.4° Plymouth MtBatten (50 m) 15.4° Lough Fea (227 m) 15.4° Prestwick (27 m)
Go to Current Weather in the selection list down the LHS, then tick dewpoint and also tick table and then set your time.












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