To many who walk down Bruce Grove, Tottenham, number 7 probably just looks like yet another old Georgian building under threat from development.
Number 7 & 8 Bruce Grove, Tottenham
Yet, if you look closely, the blue plaque says that the Grade II listed building was once the home of Luke Howard, ‘namer of clouds’.
The once grand Georgian villa was given permission to be developed over two years ago yet the developer has so far failed to begin the conversion. The building has since fallen into an alarming state of disrepair.
The petition is targeting 2,000 signatures
A petition has been set up to pressure the developer to take action before the fabric of the facade is lost forever.
Howard’s system of naming clouds is still in use today and his studies of the capital’s climate, using observations made at Tottenham and his former home in Plaistow, contributed immensely to our understanding of the urban heat island effect.
The blue plaque was unveiled in April 2002 at a ceremony attended by the BBC Weather presenter Michael Fish and Luke Howard’s descendants
His diary entries, including accoubnts on inundations from the River Lea, are also important in terms of our understanding on how severe weather in the early 19th century impacted London. He also had an influence on how Constable went about capturing the mood of a painting through careful cloud study
In terms of significance, Number 7 Bruce Grove is up there with 62, Camden Square, NW1, where George Symons pioneered the scientific study of rainfall, setting up the British Rainfall Organisation.
Chesterton House, Balaam Street, Plaistow, was the home of Luke Howard in the early 1800s before he moved with his family to Bruce Grove in 1813. Top pic: LB Newham
Too much of old London has already been lost. By reminding Redwing Estates of the importance of this small corner of Tottenham we might just help stop Howard’s former home going the same way as his Plaistow abode that was demolished to make way for an ambulance depot decades ago.
You can sign the petition at: https://you.38degrees.org.uk/petitions/save-7-bruce-grove-tottenham
The run up to Christmas 85 years ago saw yet more terror in the form of Luftwaffe bombs falling on an already shellshocked population in east London.
The final raid of the year, on the evening of December 8th, saw yet more tragedy befall the borough of Woodford.
Just after 7pm a high explosive bomb fell in St Albans Road, killing three people. And at 10.25pm a paramine was dropped on Wordsworth Avenue, South Woodford, killing 14 people and injuring 41.
It was the second deadliest day of the Blitz for the two boroughs which had already endured three months of bombing raids that had left 27 dead and over 100 injured.
The weather was fairly typical for early December, some winter sunshine with a high of 6C followed by a minimum of 2C. Really cold weather didn’t arrive until much later in the month.
Over a period of eight months around 450 bombs were dropped on the two boroughs, killing 129 people and injuring 194.
When I was writing up my winter forecast I came across an analogue that was very similar to what happened during the period November 10th to December 31st.
The period November 10th – December 31st in 1806 and 2015 show some striking similarities. It is also notable that mean during 2015 was 3C higher than 1806. Is this a question of synoptics or a warming world?
The results showed a close similarity between the two periods, November 10th – December 31st, though the mean in 2015 was some 3C warmer than 1806. Is this a question of synoptics or is this area now 3C warmer than it was just over 200 years ago?
Rainfall was also remarkably similar: 87.7mm fell from 10/10 – 31/12, just over 5mm more than 1806.
The period November 10th – December 31st in 1806 and 2015 show some striking similarities. It is also notable that mean during 2015 was 3C higher than 1806. Is this a question of synoptics or a warming world?
Luke Howard, in his first volume of The Climate of London, describes a very warm December that followed on from a warm November that fooled flora and fauna into thinking spring had begun early.
Howard’s statistics are very high: a November mean of 9.5C while December was 7.2C. CET that November was 2.3C above average while December was 3.3C above average. Considering the England Wales Precipitation series a slightly wetter than average November was followed by a very wet December – over 250% the monthly average.
“The catkins of the filberts expanded prematurely. On December 25th a hedge sparrow’s nest was taken at Doveridge, Derbyshire, with four eggs and near Warwick a green linnet’s with two eggs. It is worthy of remark that the heat was the same on December 24th as on June 24th last – on both those days the thermometer being nearly 60F.”
Howard goes on to describe how the south-west wind had “reigned for weeks” – for most of November and December before finally giving way at the turn of the year.
“The south west wind which had so long reigned yielded just at the close of the year to the north and west . Some frost ensued which, however, had not the characters of permanence being neither ushered in by driven snows nor accompanied with a dry and serene atmosphere.”
The period November 10th – December 31st in 1806 and 2015 show some striking similarities. It is also notable that mean during 2015 was 3C higher than 1806. Is this a question of synoptics or a warming world?
His description is not dissimilar from what is known as a “three-day toppler” cold spell where a dominant European high briefly gives way to cold air from the north-west or north, bringing often heavy snow to Scotland and the north but just a few cooler days in the south, before the cold feed is cut off as the high re-establishes itself.
Howard also describes how the warmth affected plants.
“The effects of the late high winter temperature on vegetation must have been obvious to everyone who has seen the country. To the very close of the year the grass continued to grow, the daisies to enamel the turf and many of the inmates of our gardens native and exotic to thrive and blossom. Even hyacinth bulbs left in the open beds shot up and flowered. Ten years ago winter came on six weeks earlier and with considerable severity.”
Words that echo what’s going on this month, particularly in the south-west where I’ve heard reports of roses still in bloom and affected by greenfly whiles daffodils look like they will be out in a couple of days.
January and February 1807 were, by the standards of that time, roughly average.
Tornadoes, earthquakes, heavy rainfall, abnormally low temperatures, pea-souper fogs and exploding meteors are phenomena that marked the Year Without a Summer around the world 200 years ago. But how did London fair?
The monthly anomalies of the two years closely follow the same pattern between March and August
When extreme weather affects Britain, such as the floods plaguing northern England and Scotland, conditions in the capital are benign by comparison.
There is not a great deal written in the press about the weather in London in 1816. So, as ever, Luke Howard’s The Climate of London, is a primary reference point.
After a wild end to 1815 that was marked with snow and lightning 1816 started dry, cold and frosty. Though cold by today’s standards January 1816 was fairly average and much warmer than the previous two when the last Thames frost fair was held.
The highs and lows of 1816 and 2015 compared
Though the temperature reached 10C on 10th the rest of the month was marked with maxima around 6C and the odd frosty night.
Cold weather returned at the end of the month, turning severe in the second week of February. In the early hours of the 7th heavy snow, driven by gale-force north-easterly winds, brought possibly some of the worst winter weather this area has ever seen. Some 35mm of precipitation is recorded on the 8th – this would normally give at least one foot of level snow that could obviously be whipped up into huge drifts.
Luke Howard described the scene in his diary entry saying the abundance of snow “loaded the trees to their tops and weighed down the smaller shrubs to the ground.”
The snow and polar continental air also produced perfect conditions for a textbook radiative cooling night. The minimum recorded on the 10th: -20.6C has not, as far as I can tell, been repeated since.
To put that into perspective the lowest minimum of the severe winter of 1963 for this area was -12.2C recorded at Greenwich on January 21st. The coldest night I have personally recorded was -10.3C on January 12th 1987.
As often happens with severe cold snaps Howard reported on the 17th the the snow “was mostly gone but very thick ice remains on ponds”; a period of just under a week.
The cold snap saw the mean temperature for February over three degrees colder than average at 0.8C.
As well as keeping meticulous observations in Plaistow, Stratford and Tottenham, Howard always kept an eye on what was going on abroad and noted that earthquake activity was high.
On February 2nd an earthquake that ‘lasted nearly three minutes’ was felt at Lisbon. Three days later an earthquake was felt on Madeira.
“At midnight a severe shock of an earthquake was felt all over the island and the following morning at 4 o’clock another shock was felt.”
An extract of a letter from Captain Welsh of the Claudine described an event of an earthquake felt at sea on the 9th.
On the 9th of February off St Michael’s we experienced very tempestuous weather with a tremendous confused sea. The wind shifting from SW to SE and NE with constant lightning and heavy rain. On the 10th at 8.30pm, the ship then under reefed fore sail and mainstay sail, we were much alarmed by a severe shock of an earthquake which lasted four or five seconds.
The dominant wind direction in 1816 was north-west
Later in the month on 23rd it was reported that the snow in the Grampian hills was at its greatest depth for 20 years.
Howard reported a heavy short snowstorm in the capital on March 4th. He also mentions another earthquake on March 17th that affected the north of England in towns and cities including Doncaster, Bawtry, Blyth, Carlton, Worksop, Sheffield, Chesterfield, Mansfield, Nottingham, Lincoln and Gainsborough.
“A smart shock of an earthquake was perceptibly felt in Lincoln at about 12.50pm. The undulation appeared to be from west to east and lasted from about a minute and a half to two minutes.
“Pictures and other articles hanging on the walls were set in a swinging motion. At Newark also and the neighbouring villages the shock was distinctly felt as well as at Leicester and Loughborough.”
Snowy episodes in the capital lasted well into April. On 12th snow fell for two hours “turning the high ground of Hampstead in the distance white”.
Very high tides were reported on the 15th with “much water out in the marshes”. By the 19th it was noted that the growing season was being severely hampered by the cold weather
April 1816 was nearly 1.5C below average. Despite this, by the 21st, the first swallows began to appear.
May and June were again cold. More than twice the average rainfall in June suggests the weather in the sixth month was very disturbed.
On the 25th a tornado, strong enough to carry objects weighing 60lbs, was reported in the Edgware Road area.
At two o’clock being a still sultry day a whirlwind passed over the nursery ground of Mr Henderson in the Edgware Road which lifted seven lights from the greenhouses and carried them to the height of the highest elm trees, each of the lights weighs 50 or 60lbs at least. At the same time two garden mats were carried to an immense height so that the eye could not distinguish them.
The following day “extremely heavy and prolonged rain from 9am (26th) to 9am on 27th gave 2.95 inches”. This total of over 52mm is notably high though not a record.
Overseas, meanwhile, the weather continued to confound observers. Several inches of snow fell in Quebec on June 8th while a letter from a friend of Howard mentioned a reading of -38F that had been recorded in New Hampshire earlier in the season.
July and August were similarly cold and wet. While events in London had quietened down Howard noted that the Kendal Chronicle was reporting snow on the summit of Helvellyn on July 4th while notable gales in Scotland were affecting ships.
More earthquakes shook locations around the world including one on August 14th in Scotland that caused panic and considerable damage in Inverness. Howard quotes a letter from north of the border:
“Last night, exactly a quarter before 11 o’clock the town of Inverness and the surrounding country was fearfully shook by an earthquake. We fled to the street where we found almost every inhabitant; women and children screaming and a very considerable portion of them naked. Many fled to the fields and there remained for the greater part of the night. Chimney tops were thrown down or damaged in every quarter of the town. The Mason Lodge occupied as an hotel was rent from top to bottom, the north sulk of the chimney partly thrown down one of the coping stones weighing, I should think, from 50lb to 60lb, was thrown to the other side of the street a distance not less than 60 feet.”
Elsehwhere in Europe the dreary summer and frequent thunderstorms inspired Mary Shelley to write Frankenstein. A summer vacation in Switzerland led her to spend much of the time indoors. She, along with Lord Byron and John William Polidori entertained each other with a contest to write the scariest story of all. The unseasonal conditions, along with this dare, led to the creation of Shelley’s Frankenstein: The Modern Prometheus— as well as Polidori’s novella The Vampyre and Byron’s long-form poem, The Darkness.
Though it is known as the Year without a Summer 1816 was actually only the 8th coolest summer in the local series going back to 1797. There were also 21 wetter summers – the 250mm that fell was actually less than half the rainfall of summer 1960.
1816 & 2015 compared: monthly rainfall anomalies
A change of month in September failed to bring a change in the weather and the mean temperature continued 2C below the average for the period. Howard mentions a 9-week tour of Europe at this time – his laboratory and climate reading duties left in the hands of his friend and partner, John Gibson.
Howard’s account of his tour explains how excessive summer rains had made life difficult from Amsterdam to Geneva.
“From the sources of the Rhine among the Alps to its embouchure in the German ocean and through a space twice or thrice as broad from east to west the whole season presented a series of storms and inundations. Not meadows and villages alone but portions of cities and large towns lay long underwater; dikes were broken, bridges blown up, the crops spoiled or carried off by torrents and the vintage ruined by the want of sun to bring out and ripen the fruit.
“While the middle of Europe was thus suffering from wet, the north for a time and to a certain extent was parched with drought and public prayers appear to have been ordered about the same time at Riga for rain and at Paris for sunshine.”
On September 16th Howard noted that a ‘dreadful’ hurricane had affected the Caribbean island of Guadalope. “Houses were levelled, plantations destroyed and the soil driven about like dust in a whirlwind.”
October 1816 was a blip during 1816 in that the mean temperature and rainfall were about average though Howard’s records reveal there were four air frosts.
By November the weather began mild but by the 6th the cold had returned with a brief snowy snap. A report from Chester said that day was almost night because of the thickness of the cloud:
“Candles or lamps were obliged to be lighted in all the houses this was succeeded by a slight shower. On Thursday successive falls of hail and rain took place. On Friday the frost was uncommonly severe and on Sunday the snow which fell was above 2ft deep in the streets.”
On the 14th reports came from France that a tempest on the night of the 11th and 12th had wrecked many ships: “winds blowing from the north then SSE”.
Chesterton House, off Balaam Street, Plaistow, was the home of Luke Howard from 1806-13. The building has since been demolished
A solar eclipse on the 18th was followed by a sustained build in pressure from the 22nd with fog now becoming a problem in the capital.
The Evening Mail on November 27th reported that the problem was particularly acute in South London.
“The atmosphere was so darkened yesterday morning in the vicinity of the metropolis by the thick fog combined with smoke that in some parts it appeared like a cloudy night. In the neighbourhood of Walworth and Camberwell it was so completely dark that some of the coachmen driving stages were obliged to get down and lead their horses with a lantern.”
After the average October November had reverted to type and the month in London finished just over 3C cooler than average.
Pressure began to fall with the arrival of December. On the 12th reports of a meteor were made from Glasgow and Perth. The phenomena sounded spectacular:
“The meteor made its appearance in the SW in the form of a small star and gradually increased in magnitude till it reached the zenith when it subtended an angle nearly equal to that of the full moon. In shape it resembled a paper kite. After passing the zenith it again seemed to diminish in size owing no doubt to its gradually receding from the observer till its altitude was equal to about 30 miles when it exploded like a sky rocket. The report of the explosion, which is described as more tremendous than the noise of the loudest thunder, reached the ear about three minutes after the meteor vanished so that it could not be less than 40 miles distant and probably about 27 miles above the surface of the earth. From the various particulars collected its diameter must have been about 240 yards. The light which it yielded was very considerable being sufficient to render the smallest objects visible.”
Two days later the air pressure fell to its lowest point that year: 966.1mb. In the early hours of the 15th Howard wrote of an earth tremor that lasted 15 seconds.
A brief cold snap arrived on the 19th with the temperature falling to -10C on 21st – by the 26th, however, the temperature reached 10C.
Though December was relatively milder than November the month still finished 1.5C below average with 1.5 times average rain.
1816 & 2015 compared: East London maxima1816 & 2015 compared: East london minimaEnter 1816 & 2015 compared: East London rainfall
The climate of London can vary greatly to figures revealed in the Central England Temperature series. Because this dataset covers an area of the UK enclosed by Lancashire, London and Bristol the resulting monthly mean temperature can often be quite a bit lower than what is experienced in the capital.
Though these anomalies are smoothed in the monthly series that stretches back to 1659 notable daily extremes that happen nationwide tend to get lost. One example was earlier this month when the UK’s November maximum temperature record was broken. Trawsgoed in Wales reached 22.4C on the afternoon of the 1st whereas a largely foggy east London recorded just 11.5C.
Comparing CET with data from Greenwich back to 1850 reveals a gradual decoupling between the two series, the warmth of London’s urban heat island effect an ever-growing influence.
The 1851-1880 30-year average means show that Greenwich was 0.6C warmer than the CET series. By 1981-2010 this gap had widened to 1.2C – indeed the London series is today 1.4C warmer than it was in 1851-80 whereas CET has warmed by only 0.6C.
Delving further into the data reveals an increase in the number of times that the 30-year average mean is being breached by at least 1.1C. The period 1961-90 was the warmest in both cases with the mean being breached by 1.1C or more on four occasions in the case of CET and five in London. It is interesting to note, however, that the largest anomaly in the CET series is 1.3C in 1921, greater, albeit by only 0.1C, than the warm years of 1990 and 1999.
The largest anomaly in London, 1.6C, was set in 2011, 0.1C higher than 1999, 1997 and 1989.
The graph below shows the number of occasions that the 30-year average has been exceeded in each period by 1.1C or more. With 1961-90 being so warm it appears that CET warming has slowed though it should be borne in mind that we have another five years before the 1991-20 series can be released.
With reference to the London graph below showing the number of occasions that the 30-year average has been exceeded in each period by 1.1C or more merely confirms that the level of the anomalies have increased but, as already mentioned, there are probably far more outside influences affecting the outcome such as UHI, population growth, further industrialisation etc.
The accelerated warming is a worry in terms of how London would adapt should summer temperatures greatly increase, though, of course, it remains to be seen if the anomalies will advance even further from current levels.
Global temperatures are on the rise though our part of the globe may not be as adversely affected as elsewhere.* The CET dataset is the longest instrumental record of temperature in the world. The mean, minimum and maximum datasets are updated monthly, with data for a month usually available by the 3rd of the next month. A provisional CET value for the current month is calculated on a daily basis. The mean daily data series begins in 1772 and the mean monthly data in 1659. Mean maximum and minimum daily and monthly data are also available, beginning in 1878.
This table shows the stats for Greenwich during spells when there has been heavy snowfall somewhere in the south-east. The figures reveal that it is very hit and miss and that the associated air doesn’t stay cold for long. There is a link to UK-wide November snowfalls here: http://1drv.ms/1PjOB9H
November has produced some potent snowfalls in Scotland and northern England over the past 150 years. These brief shots of cold air, often direct from the North Pole, however very rarely produce anything that can sustain long-lasting low-level snow in London and the Home Counties.
With the GFS weather model occasionally hinting at a blast of polar maritime air I decided to have a look back through the records to see how frequently the capital has turned white during the eleventh month.
Anyone who is familiar with the Objective Lamb Weather Type (LWT) data series will know that there may be an increased likelihood of things turning colder at some point this month. Last month was the joint 5th most anticyclonic October in the LWT series data series that runs from 1871; resulting stats closely resemble both October 1946 and 1962 as being very anticyclonic. Another similar year is 1972.
November 1972 was mild till mid month and then turned much colder with snow in places. November 1962 was cyclonic till the 24th, and then anticyclonic, with a cold northerly outbreak from the 18th for a few days with snow, before turning rather mild. November 1946 in complete contrast to both years, was a mild, dull and very wet month.
The most impressive November snowy spells seem to have occurred in the late 1800s. These two 500mb reanalysis charts show a cold feed from Scandinavia in both cases.
Snow and sleet falling in the London area is obviously much more common than snow lying. The snowiest Novembers were in 1919 and 1952 when snow or sleet fell for 10 days at Wallington and Hampstead respectively.
Kew saw snow or sleet on 8 days in 1919, while Heathrow and Northolt recorded snow or sleet on eight days in 1952.
This small article appeared on the front page of Reynold’s Newspaper in November 1890
The only decent snowfall that occured in London in my lifetime was November 1993 – and I was abroad for that. I remember my dad mentioning it in a letter written to me as I travelled round China. It arrived in the early hours of one Sunday morning and fell to a depth of five inches.
Given that was the last time London saw a decent fall I won’t be holding my breath that we’ll see any this month – though, if you live in Scotland, the odds are much narrower.
Before 1861 information on snowfalls becomes scarce – at least in terms of correct quantity. However, heavy snowfalls obviously did occur. On November 17, 1816, the Inverness Journal contained this report:
“The winter has commenced with a severity almost beyond example. Frost, rain and snow have been almost incessant during the last week and the greater proportion of corn still uncut or in stocks has suffered material injury.
“We regret to say that several lives have been lost. A postboy of Bennet’s coming from the south was obliged to leave his chaise on the road and would have been lost but for the lights shown from the windows of Moyhall which he reached nearly in a frozen state. The obvious advantage of keeping lights in stormy nights in the windows of houses in the country has thus been illustrated
“The winter it appears has set in with extreme severity in the interior of the continent. At Augsburg on the 19th of November the eclipse of the sun was entirely obscured by a fall of snow which commenced at 7 o’clock in the morning and lasted till noon. The ground was covered with snow a foot in depth. There was a great fall of snow at Frankfurt on the same day and Reaumur’s thermometer showed at from 9 to 10 degrees below the freezing point.”
Perhaps the most impressive, modern day snowfall in the south of the UK occurred around November 18th 1972 when observers recorded 60cm of snow on Dartmoor. Synoptic charts and other data are attached below.
Image courtesy of the Met Office
Image courtesy of the Met Office
Image courtesy of the Met Office
Image courtesy of the Met Office
Inspiration for this piece came from Dr Richard Wild’s PhD study on snowfall which you can find here.
Geoffrey Prater served in the 51st Royal Tank Regiment during his five years’ national service and saw action during World War II in Italy and North Africa.
I met the 91-year-old Wanstead resident earlier this year after my article on the Blitz prompted him to write to the editor explaining what life was like during the war 75 years ago.
Over a cuppa we spoke at length of how he and his family coped with the Blitz. Carefree days spent playing over Wanstead Park and Wanstead Flats were brought to an end in September 1940 as the Luftwaffe’s bombs started to rain down. In November 1940 Geoff lost his elder brother, Doug, during an air raid in Stratford.
He was called up for national service in September 1942 and, after a year of training at Brentwood, Farnborough and Barnard Castle, his regiment set sail from Liverpool docks in December 1943. Five days on mountainous seas, through the Bay of Biscay, ended with arrival in north Africa on Christmas Day from where he was posted to Italy to fight the Axis.
On returning from Italy Geoff had to come to terms with the fact that his family home in Devonshire Road, Leytonstone, had been destroyed by a V1 doodlebug bomb. His mum and younger brother, Dunc, who only narrowly escaped the bomb, had to move to a flat above a shop in Chobham Road, Stratford.
Geoff has written an account of his experiences during World War II. It’s an absolutely fascinating read and is available both in paperback and download here.
I feel privileged to have met Geoff. We owe so much to his generation’s fortitude and courage in the face of adversity.
In his own words, from the introduction of his book:
“Most people of my generation are proud to have been part of those momentous days, whether in the Services, or at home. They all suffered the grim hardships that existed at that time, with determination to see it through, whatever the cost. So, next time you see some old boy, walking down the road wearing his medals, usually at November time, don’t say, ‘Look at that silly old fart’. Just respect his pride in wearing them, after all he might be one of those ‘old boys’ who saved your way of life.”
Between 2mm and 3mm is estimated to fall between 6pm and 9pm . Fog cancelled fireworks organised for Wanstead Flats on Sunday
Bonfire Night celebrations are looking a bit damp tonight with rain spreading in just at the time many will be looking to light the fuses of fireworks as darkness falls.
According to the Euro4 model revellers can expect light but steady rain between 6pm and 9pm – annoying given that Sunday night’s festivities on Wanstead Flats were cancelled thanks to thick fog forming during the late afternoon as the sun began to set.
Wanstead Flats has put on some spectacular Guy Fawkes’ nights over the years. I didn’t realise quite how many years until I stumbled upon this old British Pathe clip which shows nurses at Wanstead Children’s Home building a huge bonfire for the children in 1934.
The footage shows the nurses struggling to get the Guy atop the bonfire, using numerous ladders, while the children, including 12 sat in an old perambulator, look on. The stats for the day reveal that the temperature fell to a chilly 2.7C after a day high of 7.9C. There was also some drizzly rain, though less than 1mm.
The Aldersbrooke Childrens Home for Waifs & Strays is still there in Brading Crescent on the Aldersbrook Estate, although the five lodges have been converted to flats.
In 1907, the West Ham Guardians purchased the Aldersbrook site. In 1911, five receiving homes were completed. The homes were called lodges and were: Elizabeth Fry Joseph Lister, Tom Hood, Edward North Buxton and William MorrisA bit of history…
In 1913, a workshop, for training of the older boys and girls was opened. Skills learnt were in tailoring, carpentry, laundry work and needlework, under skilled industrial trainers.
In 1930, on the 1st April, the ownership of Aldersbrook homes and the leases of the Scattered Homes, were under the 1929 Local Government Act, and by agreement with the Essex County Council and the West Ham Corporation, vested in the East Ham Corporation who are required to continue to receive destitute children from the Essex County Council and West Ham, formally comprised in the West Ham Union area.
On 27th May 1933, the Aldersbrook Children’s Homes new nursery was opened. The County Borough of East Ham owned it. Alderman T.W.Burden, Chairman of the Public Assistance Committee, opened it. The Mayor of East Ham, Alderman G.H.Manser J.P, proposed a vote of thanks, which was seconded by Alderman C.W.Brading J.P, and supported by Alderman Mrs Taylor (East Ham) and Councillor G.Doherty, of West Ham. After the official opening, the older children (14 to 16 years old) of the homes put on the play “David Garrick”.
The superintendent of the home was W.T.P. Steele, and the matron was E.M.Steele. S.R.N. The building was described as being divided into three sections – ground floor, babies under twelve months and toddlers one to three years, first floor staff. Accommodation is given for ninety infants under three years. Wards are provided for these age groups were newly admitted children will be housed for three weeks before being sent to the general rooms. Two ranges of isolation rooms are also provided where “suspects” can be nursed to reduce the risk of infection. The south end of the building is allotted to the youngest or cot babies and comprising of long dormitory with sun rooms at the end, designed to catch the winter sun.
The former Aldersbrook Children’s Home is still there in Brading Crescent but has been converted to flats
The programme went on to describe the building as being the most modern of children’s institutions. The building has a veranda at the front. The first floor has 21 separate staff bedrooms. The building had an oil fired heating system and flooring with fire resistant Terazzo material whilst the children’s play room and dormitories are protected by rubber flooring. The lighting and power points are controlled by locking device to prevent the children switching them on and off. The building was built by Messrs Hammond & Barr Ltd Chelsea.
The Nursery is now gone and the Aldersbrook estate covers the area, although the recreation Hall, the lodges (See photo) and the porters lodge are still there.
The incident of frosts during the season from October to May. There has been a general uptick overall since 1999/2000
1934 and this year, together with the last couple of years, is a far cry from my memory of Bonfire Night being a frosty affair – despite the fact that frosty nights during the season from October to April have been showing an uptick since 1999/2000.
The synoptic chart on November 5th 1934 portrays an unsettled regime
The synoptic chart from 7am on November 3rd 1940 showed a deep depression crossing the country that brought over 40mm of rain to Greenwich Image: Courtesy of Met Office
November 1940 was the wettest on record for this area. Over 170mm of rain fell in Greenwich, beating the previous record set over a hundred years before in 1836.
Other areas of London were even wetter: Croydon was wettest with just under 196mm while Addington recorded just under 194mm, Bromley 179mm and Regent’s Park 175mm.
Nearly a quarter of the month’s rainfall fell on the 3rd. The total of 40.8mm is a daily November record that remains to this day. Indeed, throughout the month, there were falls of more than one inch (25.4mm) somewhere in the London area on four days: 40.8mm (3rd, Greenwich), 26.7mm (4th, East Ham), 26.4mm (11th, Camden Square), 27.4mm (13th, Southgate).
In Wanstead and Woodford the inclement weather coincided with a 6-day pause in bombing incidents during the Blitz. November was a very cyclonic month that probably hampered German air operations.
Another 6-day pause in the bombing happened after November 16th. When the Luftwaffe returned on Saturday, November 23rd, it was Wanstead that bore the brunt. At 4.12pm, as light was fading on a dull, dreary afternoon, high explosive bombs caused fires at and partly demolished nos 78 and 89 New Wanstead. A minute later another bomb ruptured water and gas mains in Spratt Hall Road. At 4.30pm a further high explosive bomb fell in the High Street, killing 4 people. The raid ended at 5.16pm as a bomb fell in Fitzgerald Road though this time there were no injuries.
By now the weather was beginning to quieten down though weeks of deep depressions with associated gales and heavy rain had taken their toll – many residents reported problems of Anderson bomb shelters being constantly flooded – but it was probably the design as much as the weather that was to blame.
As pressure built in the last few days of November the first frosts of winter arrived but the bombs returned. High explosive devices fell in Woodford New Road and Bunces Lane on the 30th, fracturing a water main.
To put November 1940 into some sort of perspective the average fall for the month in this area, with regard to the 1981-2010 average, is 59mm. The closest this area has come to matching the record was 2009 when 150mm was recorded and preceded a cold winter.
The following synoptic charts are for each day of November at 7am. All courtesy of the Met Office
Every so often the UK experiences severe weather which shocks a population that is very used to our mostly benign climate.
Newspapers and media agencies, in an age where a culprit must be found to blame, are quick to connect every gale, flood and snowstorm with climate change. To say it is just ‘weather’ doesn’t compute with the average news editor.
The year 1868 saw months of extreme weather that led newspapers on a mild and rain-sodden Christmas Eve to first ask the question: ‘Is our climate changing?’
A look back through archives from the 19th century reveal that this is not a new phenomenon. Though extreme weather events, including the heatwave of 1808 and widespread floods of 1811 and 1828, were always well documented, it wasn’t until the advent of reliable meteorological readings in the mid 1800s that scientists could analyse what was happening to the atmosphere with any authority. This, coupled with an explosion in literacy rates and the British fascination with the weather, helped build an appetite for news stories that went beyond covering each gale, flood and blizzard.
The year 1868 saw months of extreme weather that led newspapers on a mild and rain-sodden Christmas Eve to first ask the question: ‘Is our climate changing?’ The year had been the warmest for 34 years. The CET mean for 1868 was 10.4C, a figure nearly 1.3C above the 1831-1860 average. To put that into perspective 2014 was only 1C above the 1981-2010 average.
A review of weather in 1868 in the Falkirk Herald said the year had started very wet – a farming diary kept in Connaught, Co Mayo, said that January was so wet it was impossible to plough the land. The very wet weather lasted until the last week of March. In the Armagh record, all three months had well-above average rainfall, with the three-month total of 363 mm representing around 180 per cent of the long-term average.
By contrast the summer of 1868 was very hot and dry, with some of the highest temperatures ever recorded for the second half of July occurring in this year. There was a remarkable spell of hot days, with temperatures over 30C in England. For the south-east specifically, a maximum temperature above 32C was recorded in each of the months from May to September, and in July, the temperature exceeded 32C on 9 days. It was regarded for many years, until 1976 at least, as the longest (because of a lack of rainfall) and hottest in the instrumental record for England.
Although not accepted under modern methods, because of problems of comparison between Glaisher stands and Stevenson screens, the maximum temperature recorded on July 22nd, 1868 at Tonbridge, Kent, is still remarkable: 100.6F (38.1C). It is thought that this value, when compared with a standard Stevenson screen, is about 1.5C or 2C too high.
The subsequent ‘standard’ winter (December, January and February) became the warmest winter in the CET series which began in 1659, a record that still stands today.
The mild temperatures suggest a highly zonal, westerly pattern held sway from late November 1868 until at least February 1869. Snow was scarce in 1868 – with the only heavy falls on March 3rd and 8th and November restricted to northern England and Scotland.
Gilbert White, in his journal Natural History of Selbourne, tells of a visit to London in January 1776 when the metropolis was completely embedded in snow. He says that snow remained on houses in the City for 26 days – these days it is unusual for any snow to fall in the centre
The Falkirk Herald goes on to point out that winters, for the past 25 years, were mostly mild and wet – any bitter spells were short-lived. The piece cites Gilbert White’s Natural History of Selbourne which tells of a scene in January 1776 when “narrow roads were filled with snow to the tops of the hedges”, stopping road wagons and coaches in their tracks. White, regarded as England’s first ecologist, remarks that on a visit to London on the 22nd the metropolis was completely embedded in snow. A frost on the 27th lasted four days and was so intense that the Thames froze sufficiently enough for crowds to run about on the ice. More tellingly the snow remained on houses in the City for 26 days – these days we’re lucky if we see snow fall at all in the centre.
The paper professes that an increased occurrence of gales in mild winters were preferable to the ‘wave of death’ that accompanies bitter winters:
To the strong and hearty the frosts and snows of a bitter winter may seem genial and invigorating ; but they bring death with them to the weak, the ailing, and the aged.
It had been nine years since Charles Darwin published On the Origin of Species and many people were starting to turn away from the popular theory that many weather disasters were the work of God.
Nine out of ten of the warmest years have occurred since 1989
Less than 5 years later the question ‘Has our Climate Changed?’ was being asked again. An article in the Fife Herald on January 30th, 1873, reported that winters were milder and that summers were colder – less frost and snow and much more rain. The month had been mild, nearly 2C above the 1841-70 mean, but the rain was more notable: 80mm, 136% of the EWP average. The wet January was a continuation of the previous 12 months which had been the wettest on record: 1284.9mm, a record in the EWP series that remains to this day. There has been a wetter 12 month period just once – April 2000 to March 2001.
The wet conditions extended across Ireland too; in the Armagh record, the 12 months from February 1872 to January 1873 saw 1251 mm of rain fall, which represents about 150 per cent of the long term average for this station. A farming diary in Connaught, Co Mayo, stated that the persistent wet weather caused considerable distress through loss of harvests and difficulty of working the land.
By the time the question: “Is our climate changing?” was asked again, 16 years later, the climate had turned much colder with the return of snowy winters. Snow fell on 16 days in February 1889 – a storm on the 10th and 11th dumped 20-30cm of snow widely across England. Days later the Hull Daily Mail reported a statement by Professor Cleveland Abbe which said that the climate of the earth had not changed in 2,000 years.
The comments of Professor Abbe, today considered the father of the US National Weather Service, were drawn from a report in the US magazine, The Forum, and referred to temperature, rainfall, early and late frosts, freezing of rivers, periods of cold winters and hot summers, the opening of navigation and the temperature of the earth. He said:
The study of each and all of these phenomena has failed to establish that there has been any sensible change in the climate at any point of the earth’s surface during the past 2,000 years.
It is not clear if Professor Abbe’s words were taken out of context but it is interesting that such a well-respected scientist had the confidence to make such a statement.
Rainfall shows a much more even spread of records through the years than temperature
The year 1888, part of a string of colder than average years that followed the huge Krakatoa volcanic eruption in Indonesia in 1883, had seen other extreme events. In July ice is reported to have disrupted the fishing fleets around the Faroe Islands, implying cold conditions at these latitudes, probably extending to at least the Shetland Isles. It was a notably cold summer; a mean of 13.7C puts it just outside the ‘Top 10’ of coldest summers in the CET series. In London the summer was 1.8C cooler than average and rainfall was 139 per cent of normal for that period. It was also the dullest on record.
Two decades were to pass before the question: ‘Has our climate changed?’ appeared again following a fairly mild and wet winter. The Dundee Courier, on April 9th 1908, suggested that winters had grown milder but admitted there was no known cause. It said that the Thames had not frozen over for nearly 100 years but that this was partly caused by the fact that London Bridge was replaced 80 years previously, totally changing the tidal flow of the Thames.
Five months later a soggy Dublin Horse Show prompted the Wells Journal on September 10th to report on findings by the meteorologist Sir John Moore featured in the Geographic Section. He looked at Rev William Merle’s writings from the 14th century and observations made in Greenwich from 1774.
The facts prove that within the last six centuries at all events appreciable change has taken place in the climate of the British Isles. There is no scintilla of evidence to show that such change has taken place in the past or is likely to take place in the future.
On Boxing Day 1908 the Gloucestershire Echo cited an ancient weather report featured by Sir John Moore. In 1341 the month of April saw continuous frost from 6th to the 13th while the following autumn saw spring-like weather persist from September to December: “Our climate hasn’t changed in 600 years.” was the claim.
A poor summer in 1909 that began with the coldest June for over 230 years once again prompted the question ‘Is our climate changing?’ to be asked again by the Wells Journal on August 5th, 1909. The report says that the climate of Europe is growing colder – with periodic cold summers. It goes on to say that cold summers have happened in the past, mentioning the following years: 820 (cold and wet – most crops perish), 1033 and 1044 (cold and wet, caused famine), 1151 (rain falls in France continuously from end of June to middle of August), 1219, 1315, 1423 and 1512 (cold and wet summers) – in 1512 several people, accused of causing bad weather, were burned at the stake. Other years: 1596, 1639, 1641, 1667 – all had very cold Junes. The years 1809, 1812, 1813, 1816 all had cold summers.
Around the country there were some notable readings. On June 6th a high of just 10C was reached in Oxford and Bath. It was notably cold and wet with significant thunderstorms from 10th to the 12th and 20th to 28th. In London the Trooping the Colour ceremony on 24th was cancelled because of poor weather – one of only four occasions it has been cancelled due to weather since its inception in 1895. It was also a very dull month with no sunshine at all in London from June 2nd to 6th.
The year 1911 produced more remarkable weather and some violent thunderstorms. On May 31st, as the Titanic was being launched in an overcast Belfast, some 17 people were killed by lightning strikes across London and four horses died on Epsom downs on what was the day of the Derby. About 62mm of rain fell in 50 minutes on the Downs and there were 159 lightning strikes in 15 minutes around 5.30pm.
The summer season that year was the warmest for 65 years with many areas having less than half their normal rainfall. July was spectacularly sunny with an average of over 10 hours of bright sunshine over much of southern England: 384 hours of sunshine were recorded at Eastbourne and Hastings, East Sussex, during this month, and these are thought to be the highest sunshine totals recorded anywhere for July in the UK.
August 9th, 1911, saw the first incident of 100F (37.8C) being recorded in London. The record beat the previous high of 97F. The report also makes mention that many areas recorded at least 97F
For the SE of England, with something like 300-350 hours of bright sunshine, this month (with July 2006) is regarded as the sunniest month on record. The month was also exceptionally dry and is still among the ‘Top 5’ dry Julys in the EWP series. August was also warm: the 9th produced the first occasion when 100°F was recorded in London.
During the autumn of 1911, the Shields Daily Gazette on Wednesday, October 25th, was reporting that ‘weather prophets’ were predicting that the UK was in for an exceptionally cold winter. The predictions were based purely on the fact that the country had not had a bad winter in more than 15 years, the last occasion on which the Thames was partly frozen over in the early part of 1895.
“If very cold winters come on an average once every twelve years, an old-fashioned winter is certainly overdue, for there is no ground for supposing that our climate is changing. But it is not the case that cold winters follow hot summers as an invariable rule. They sometimes do so, but the contrary would seem to be as often the case, for the hot summers of 1868 and 1887, to quote two examples, were followed by comparatively mild winters.
The law of averages is certainly on the side of a severe winter this year, but in the case of the weather it is never safe to argue from any law, and as the price of coal is going up, everyone must hope that this time, at all events, the Clerk of the Weather will be merciful.
In the event the Clerk was merciful and winter was mild.
Warm winters are often thought of as a modern phenomenon but there were plenty in days past
This mild theme continued for a period prompting the Dundee Courier on Monday, January 2nd 1922 to ask: “Where are our winters? Is our climate changing?” The leading article goes on: “Here we are in January, and so far we have had no snow to speak of. Yes, our climate is changing, and has been for many years. We do not need weather records to tell us that. Our memories provide striking comparisons. In our boyhood days we greased our boots, tucked our trousers in, pulled the ear-flaps of our caps (you remember the style) down tight, wrapped mufflers around our necks (but not for fashion sake), then stood by the big fire to warm up before starting to plod our way through deep snow school.
“Who can forget the snowball battles after school; the hustle home for skates and to the ponds until nightfall; and then some? In those times we planned skating parties, and we were not disappointed. Do we need the records of thermometers and snow gauges to remind of the days of stinging cold and streets “piled high with snow ?
Anyone who says our climate is not changing has not been on this earth long enough to know. The severe winters left indelible marks upon our grandparents and great-grandparents, and the weather developed strong constitutions. They tell of successive winters of heavy snow and intense cold, beginning early in November and lasting until late in March. The snow often was piled up from four to six feet deep on the level.
There’s been far more wet winters than dry winters in modern times
“The seasons in those times were evidently well marked, for frequently made of their definite beginning and ending. Winter evidently was the season that concerned our ancestors most, for only slight mention made of any unusual summer.
In Britain the last few years winter temperatures have been higher than the average. The cold period has several times occurred in the autumn and May is showing a tendency to become the most pleasant month of the year, and so we are again reminded that the climate is changing; while statisticians say that average temperatures have remained practically the same for the last 600 years.
“A change in climate does not necessarily involve a change from the average mean temperature. It frequently happens that a warmer winter and a cooler summer or vice versa, or even a moderate winter and an unusually hot summer leave the average practically the same, while climatalogically very decided changes have taken place.”
Six years later a very poor summer prompted the Dundee Evening Telegraph on Tuesday, July 3rd 1928 to again ask the “eternal question”: Is Our Climate Changing? “With days of wind and rain that have made June and July days seem more like March and at times, even November, we are still awaiting our real summer. It is not uncommon to hear people speculating as to whether, after all, our seasons are not in process of changing.
“It is interesting, even if is not comforting, writes a correspondent, to know that people were speculating on exactly the same matter many years ago, and that in 1892 the author of Dundee and Dundonians Seventy Years Ago, when writing on Olden Rime Storms, Floods and Droughts, thought to ask: “Is our climate changing?”
Five of the ten warmest summers have occurred relatively recently
“In a climate like ours,” says the writer of that interesting little book, the weather is a never-ending topic. Warmer and Colder. I have often heard old people speak of the weather changes that had taken place since their young days, as they expressed it. The summers, they said, were then much warmer, and, as an instance, they said that barley would be above the ground in forty-eight hours after sowing. It was then, they admitted, the last grain that was sown.
The summers then were so hot that the cows could only be put out to pasture in the early morning and evening, as they were driven mad by the ‘glegs’ or horse flies biting them. Then the winters were almost arctic in their severity and length. The seasons were also more sharply divided, approaching those of Russia and North America in their rapid seasonal transitions.
“I know that many about my own age have the same ideas of what has taken place in their time. A very hot or a very cold season or two may, as we get older, come to assume the general character of that far-off time, still I cannot but think that for a good many years past there has been more of a mixing of summer and winter than was the case fifty years ago, winter now being often found in the lap of spring, and summer-like weather about the new year.
“On a New Year’s Day – I can’t remember the date – I gathered blossom from our gooseberry bushes to show to a friend.”
On February 5th 1929 the newspapers were promoting a “new series of talks entitled ‘Is Our Climate Changing'”. The first speaker was a Mr Gordon Manley of the University of Durham. The paper said that the talks, in view of the widespread interest in weather conditions and forecasts, should prove of rather more than usual interest.
Three of the ten driest summers have occurred recently though it is notable that 2012 ranks 4th wettest summer
Manley later became probably the best known, most prolific and most expert on the climate of Britain of his generation. It took him 30 years to assemble the Central England Temperature (CET) series of monthly mean temperatures stretching back to 1659 – the longest standardised instrumental record available for anywhere in the world.
In the Dundee Courier on Wednesday, July 29, 1931, a report on a recent article “Has our climate changed?” had aroused considerable interest. David Grewar, the well known Glenisla authority, who has a long experience of the glens, gives his views below.
“Such variety of opinion exists as to whether or not our weather has changed. Some say that it has, others that it has not, and that any supposed change is due to the exaggerative effects of memory. These differences of opinion do not only exist among laymen, but among scientists as well.
Making all due allowance for changed habits and the tricks of memory, the older among us are undoubtedly correct when we say that the seasons now are different from our younger days. Then our winters were more severe, our summers better; now there’s more of a levelling up between the two.
“Mere meteorological records of temperature and precipitation cannot be taken as proof of what popularity constitutes severe winter. Suppose, for instance, that a heavy fall of snow is experienced in December, and is slightly augmented now and again for the next two months, and that never more than a few degrees of frost are registered, records would represent that as a mild winter; whereas reality it would be a severe one, because the ground would be deeply covered with snow for the whole winter. On the other hand, we may have a winter of severe frost, with little or no snow, claimed as a severe one.”
Eighteen months later and the Gloucester Citizen, on Friday, January 6th 1933, asked: “Is our climate changing?” The sub heading “January mends its manners” again enquired about whether the persistent succession of mild Januaries in the present century suggested something in the nature of a change in climate?
In the French Revolutionary calendar the division of the year from the middle of December to the middle of January was the month “Nivose” or “snowy”. The Anglo-Saxons called January “Wulfrnonath” because the weather was so intense that wolves, emboldened by hunger, left the forest and invaded the villages. The Dutch used to call January “Lauw-maand” or “frosty month”.
Today, in many parts of the country, particularly in the south and west, amateur gardeners have the delightful rare experience of seeing standard and rambler roses in full bloom, primroses blooming in rich clumps, stocks, polyanthus, indeed, show off flowers usually retarded by frost until the spring.
This changing character of “January freeze-the-pot-by-the-fire” is commented upon by a writer in the current issue Nature:
“January, the coldest month of the year in England, is proverbially associated with snow and ice. During the twentieth century, however, January has not lived up to its name but has been much more open, mild and stormy. with few prolonged frosts.
“At Greenwich the mean January temperature during the decade 1921-30 was 41.3Fs, more than two degrees above normal and probably five or six degrees higher than in some of the decades of the late eighteenth and early nineteenth centuries. This persistent period of mild winters has extended over the whole of western and central Europe and is associated with a greater frequency of south-westerly winds and may almost be regarded as a change of climate.”
Within five years, in 1938, Guy Callender produced a paper that developed a theory that Earth temperatures had been rising in line with increasing concentrations of atmospheric carbon dioxide. It was the first time that somebody had made this connection: the birth of the science of man-made climate change.
If the oak before the ash…
In 1942, the Buckingham Advertiser and Free Press, on Saturday, February 21, was discussing old weather rhymes.
“The speaker gave the following to us as among the most reliable weather verses:
“Livening red and morning grey, are surest signs of a very fine day.”
“When the dew is in the grass, rain will never come to pass.”
“There was a flicker of reason, he said, in the rhyme “rain before seven, fine before eleven”.
“Is our climate changing? Dealing with the question of our climate changing Mr Pettipher observed that people’s idea that the old-fashioned type of weather had gone forever, and that some such solution as the diversion of the Gulf Stream was the cause of the winter warmth, received a rude shock in the early months of 1939 and 1940, which, with the exception of 1929 were probably more severe than anything since 1895.
“Hot summers seemed to have been rather less frequent than in years past ; but our land was not really one of perpetual fog and gloom some novelists would have us believe, nor as bad as American thought when he wrote :
Dirty Days hath September, April. June and November ; from January up to May, the rain it raineth every day ; all the rest have thirty-one, without a blessed gleam of ; and if any of them had two and thirty they’d be just as wet and twice as dirty ! (Laughter.)
“In terms of Buckingham rainfall the speaker emphasized the necessary practical value, especially to sailors, fishermen, agriculturists and sportsmen, and now to our airmen, of weather study and manv observations with regard to rainfall described the Air Ministry’s organisation of 6,000 observers in the different parts of the country, of whom he was one, pointing out that the work had been described as of “national importance” because of its practical value.
“He emphasized that it was not a dry, hot summer that caused anxiety regarding water supplies; but a dry winter season. Buckingham’s average rainfall over a 20-year period was 25.43 inches. During the remarkable thunderstorm of May 19th when the roof of Buckingham Hospital was set alight by lightning 1.01 inches fell in thirty minutes, the percentage of 2.02 inches in the hour qualifying for a place in British Rainfall for a fall of unusual intensity.”
Much has been written about climate change in newspapers and scientific papers since the war. For a long period during the 1960s and 1970s the concern was about global cooling. But this changed in the 1990s when it became scientists identified that the Earth was beginning to warm.
A search of Wiley, the publisher shows a sharp increase in incidences of articles and papers that feature climate change. It is surprisingly just how big the increase has been since the beginning of the 1990s.
Looking at the last 10 years the Financial Times mention of the phrase ‘climate change’ is much more variable, perhaps reflecting the world financial crash of 2008 when concern was deflected away from the environment and on to the economy.
Concerns over climate change today have moved on immeasurably since those first lines of concern were vented in newspapers in 1868. But the socio-economic and geo-political arguments that are associated with the science deserve a blog all on their own. The long-range models that are still being developed, together with further study of ocean sediment, ice cores, tree rings etc illustrate that there is so much more we need to learn about this fascinating subject.
News editors would do well to take a moment the next time they report a hurricane, tornado, flood or snowstorm and realise that ‘freak’ events do happen and that it is not necessarily climate change that is the cause of that particular event in time.
As Mark Twain apparently said in 1887: “Climate is what we expect, weather is what we get.”
* Articles featured in the British Newspaper Archive were referenced in compiling this blog
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