LONDON-The weather forecasters have just given us an impressive display of their skill by predicting the scale of the current high pressure zone over the UK. Overnight, Sunday into Monday, London’s Heathrow Airport recorded a barometric pressure of 1,049.6 millibars (mbar).

It’s very likely the highest pressure ever recorded in London, with records dating back to 1692. But the UK Met Office and the European Centre for Medium Range Forecasts had seen it coming well ahead of time. “Computerised forecast models run by the Met Office and the ECMWF predicted this development with near pinpoint precision, forecasting the eventual position and intensity of the high pressure area several days in advance, before it had even begun to form,” said Stephen Burt, a visiting fellow at Reading University’s department of meteorology. London didn’t quite experience the highest of the high, however. That honour goes to the southwest of Britain.

Met Office hourly observation reports recorded 1050.3 mbar at Liscombe in Devon, at 2100 GMT on Sunday evening. 1,050.2 mbar was recorded at Dunkeswell in Devon, and 1,050.5 mbar at Mumbles, in South Wales, shortly after.

None of these measurements breach the 1,053.6 mbar recorded at Aberdeen Observatory at 2200 GMT on 31 January 1902, which remains the national record, but the events of the past 24 hours certainly marked the first time for over 60 years that 1,050 mbar has been attained anywhere in the British Isles, said Mr Burt.

“The reason for the extremely high pressure can be traced back to the rapid development of an intense low-pressure area off the eastern seaboard of the United States a few days previously (this is the storm that dumped around 75cm of snow in Newfoundland),” he explained.

“In simple terms, the air drawn out from this system through the actions of a strong jet stream has to be redistributed elsewhere.

“Normally, this would happen over a much larger area of the North Atlantic, leading to the rapid development of a fairly intense anticyclone, which is not uncommon. On this occasion, the ‘excess air’ (if we may call it that) could only be redistributed over a small area because of the existence of a number of other depressions, resulting in the rapid development and intensification of an anticyclone over the British Isles.”