Wednesday, February 28, 2018

Water and Weather 2018 so far...

Cuttings montage (January)
Winter 2017/18 (Meteorologically speaking 1st December – 28th February) was bookend by snow. We started off in NE Yorkshire where snow fell on the 30th November, affecting only NE England close to the North Sea coast. At the turn of February-March, there came the Beast from the East.

In between, the weather was more varied than during the previous winter, with more rain; but it was cold at times. January was unsettled and fairly fairly mild, but February was much drier, and colder, especially at the end of the month. It felt much more like winter, and a long one, though my perceptions were coloured by homelife hassles, such as the boiler breaking down in January.


Among the more memorable weather and water incidents:

Named storms (low pressure systems) – by the end of 2017, four low pressure systems had been named by the UK Met. Office and / or the Irish weather service. 2018 began, then with E for Eleanor on 3rd January. Later that  month: Storm David (17th January; breaking the alphabetical sequence because it was named by Meteo France. Then, Fionn (affecting the island of Ireland, but not Britain. On 24th January, the latest of the season so far, Storm Georgina. February quiet; but cold on the coat tails of the Beast from the East, Storm Emma was due to roll in from the southwest, off Iberia on 1st March. Again, out of the alphabetical sequence because it was named by the Portuguese weather service, making landfall in Portugal first. All the storms named more because of the potential for strong winds than precipitation. There were other rain and snow bearing weather fronts emanating from anonymous lows.


High tides, supermoons and blue moons – two full moons in January: on 2nd and 31st. The first known as the Wolf Moon; the second a Blue Moon, being the second in a calendar month. Both were full at / near perigee, the closest point in the Moon’s orbit around the Earth. Shortly after the first one (3rd-4th January), happening just as Storm Eleanor rolled in, some high tides (see notes from our local coast). There was also a fair bit of rain, with coastal and fluvial flood warnings on both sides of the English Channel. River and sea conditions were quieter at the end of January, the pressure being higher, meaning no reprise of the earlier tidal trouble come the Blue Moon.
Pluvial / fluvial turn-around in France for much of 2017, river levels across the Channel in France had been running low all through the autumn, with high pressure in the Atlantic off the Bay of Biscay in charge.  The weather began to turn in December when storms and rain bearing fronts passed over the country and river flows began to improve. Then, in January was very wet. From  Storm / Tempête Eleanor onwards, widespread flood alerts (vigilances) affecting most of the main rivers. According to Eaufrance / Vigicrues, the flow on the Loire at Saumur was below 200 cumecs (cubic metres per second) in early December. Around Christmas is was about 800cumecs. Around the new year, it hit made it into four figures (about normal for winter), then during the week after Tempête Eleanor, it rose more quickly and peaked at around 3100 cumecs on 9th January. The Seine and its larger tributaries, meanwhile were rising slowly but surely. Later in the month, Tempête David brought high winds to NE France, Belgium and southern England. As I grumbled at the perennial winter mud around our way, it was very dull in these areas. “A star has been kidnapped!” said one regional newspaper, La Voix du Nord, meaning the Sun. UK sunshine during January was about average according to the Met. Office, nonetheless, the month had a distinctly wintery feel to it. Whereas France was exceptionally mild and wet – the wettest December-January 2 months period nationally in the record from 1959 -  the track of the jetstream meant it was cold in Scotland. A low of -13.5oC at Dalwhinnie in the eastern Highlands on 21st January. Also snow, with queues along the A82 near Glencoe on that weekend.
Crue de la Seine – with the slow and sure rise, the Seine and it’s larger tributaries, particularly the Marne, were on flood alert for much of January and well into February, even after the weather patterns had shifted and the rain had stopped. Things got particularly high during the last week of January. The flow along the lower Loire exceeded 3000 cumecs again on the last weekend – crues habituelles pour la saison, said Vigicrues.  However, there was more significant flooding affecting the Seine; the Saône and its tributary and sub-tributaries from the Jura area the le Doubs and La Loue; and the Dordogne. On 23rd, there was a vigilance rouge (equivalent to Severe Flood Warning in the UK) on the Loue. A fair bit of footage of the Doubs on Youtube, including an impressive waterfall. Most of the media attention, though was on the Seine, vigilance orange (crue importante) from at the Marne to the Manche (English Channel) by the end of the month. Numerous Youtube footage on Paris from this time, too. A photo of a woman in a rowing boat with a dog amid a flood in a Paris suburb appeared in The Guardian across the Channel on 25th January. The Metro and boat services were also disrupted. Once again, art in the stores of the Louvre had to be shifted somewhere safer. The Seine peaked on the 29th January at Paris Austerlitz at around 1672 cumecs – the peak flow on the Eden through Carlisle (Sheepmount) during Storm Desmond, December 2015, was much the same (1680 cumecs, according to CEH), the Lune and the Tyne both above 1700 cumecs. In contrast to those rivers in northern England, though, the rise was very slow, especially near the peak. It also took considerable time to subside (décrue) afterwards. A combination presumably of lots of water propagating through a large catchment and the lower Seine being very winding, with large meanders (boucles). Throughout the last week of January, the flow into the Channel was around 2200 cumecs (Vernon gauge), thanks to additional inputs from the Oise and other rivers joining downstream of Paris. With so much water coming downstream, there was a vigilance orange in the tidal Seine during the spring tides around the Blue Moon, too. The heights and flows on the lower Seine was about the same as during the June 2016 flood, according to Météo France. In Paris, the peak (5.85m) was a bit lower than in June 2016 (6.1m). There were higher floods in the last century, most notably January 1910, when the flow through Paris was around 2600 cumecs and the level 8.62m.
During that last week, there were flood warnings in England and Wales, including along the Ouse in York and the Severn at Tewkesbury; but there was no major flooding.

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Revival of the Lavant long-time-no-see. February was notable particularly for the cold, again on both sides of the Channel. At the beginning of the month, as the sun climbed higher in the sky and the days got noticeably lighter and brighter, it began to look springlike, even if it was chilly in the wind. Walking to The Trundle from Chichester on the 3rd, I was pleased to see the Lavant flowing again – long-time-no-see. As far as I’m aware, it didn’t flow at all last year; and even on the 28th December, my other half said the stream was still dry when he walked that way. Autumn 2017 had been another dry one in southern England. Though December was wetter, the rain hadn’t yet percolated through the soil to the the chalk in sufficient quantities to raise the water table. It was January’s rain which really made the difference and got things flowing again. Hints of spring, with snowdrops flowering at West Dean the following weekend and a few daffodils coming out; but I didn’t want spring to be too early or too dry as last year’s was. Thanks very much to January’s rain, the CEH and Environment Agency say in their hydrological summaries for January that the hydrological outlook has improved since the autumn, thanks to the rain in December and January. Most gauged river flows were in their normal range, including those which had been running low at the end of last year, such as the Great Stour in Kent. The nearby well at Little Bucket Farm was no longer dry. The revival of the Lavant was reflected in a sharp increase in the level of groundwater in well at Chilgrove House nearby to the west.


Nextdoor to the east, I saw the Arun was running fairly high when I looked from the train to London Victoria on 15th February. Near Pulborough railway bridge it was overflowing. This was more due to rain falling on the West Sussex Weald from about 10th February. When I went to Littlehampton on the 18th – disappointingly overcast after bright sunshine the day before, the usually sea green water was the colour of weak tea. The tidal current was very strong, as it is here even on regular, moderate tides. Though cloudy, it was one of the milder days of the month; one of the few days of the winter when I could sketch along the coast and not immediately feel cold in the wind.

Then came the really cold bit, dubbed The Beast from the East by the British media, with the coldest weather of this winter and since 2013, and in some areas 1991. Happenings in the upper and lower atmosphere over the Arctic conspired to shift the winds to bitter easterlies and north easterlies, bringing in cold air from northern Scandinavia and Russia. The coldwave was felt throughout the British Isles and northern Europe, with sub-freezing temperatures, snow and bitter wind chill. The cold began setting in during the final week of February as a very  intense anticyclone built over northern Scandinavia and extended southwestwards towards the British Isles. The jetstream diverged; with one arm moving north of the British Isles towards Iceland and the other well south, over north Africa. It continued to loop and wind, with a big tongue of bitterly cold air sticking out from Russia westwards come the end  of the month. Over Scandinavia and just north of the British Isles the normal westerly flow of the stream had reversed to easterly as it looped up into the high Arctic and diverged in mid-Atlantic. The Met. Office issued warnings for snow and ice throughout the UK, particularly eastern areas. The snow began on the night of the 26th. It missed south Hampshire, but there was snow in London, Sussex and Kent; and deeper, drifting snow in NE England and Scotland. North of the Border, they were so concerned that on the 28th, they issued a rare red warning for snow in central Scotland, including Edinburgh. The last time they issued one of those was during the floody havoc wrought by Storm Desmond in northern Britain in December 2015. Down south, meanwhile, the Storm Emma low pressure was deepening in the Atlantic off Iberia and heading northeast across Iberia, western France and towards southern England. With its associated  fronts coming in from the south across the Channel meeting the cold air, the potential, then meant snow, ice and freezing rain round our way to start off March – the beginning of spring meteorologically speaking, even if far from the reality.


Everyone who’d rather anthropogenic global heating wasn’t happening, or denying it altogether may this kind of winter chill reassuring, bolstering the deniers’ case. . But it’s a false reassurance. All the time Britain and the continent were under a cold wave, the Arctic was getting worrying warm, thanks to. Analagous to leaving the fridge door open and letting the cold air flow out into the kitchen; the fridge here being the Arctic / North Pole; and Britain / Europe being the kitchen. Bucking the trend of the rest of the British media, The Guardian led with Arctic heatwave triggers climate meltdown fears on 28th. The warming has involved the upper and lower atmosphere over the Arctic. On the 9th February, the Met. Office said in a news release that they were forecasting a Sudden stratospheric warming in the high atmosphere over the Arctic the following week, involving an increase in temperature of as much as 50oC associated with the polar vortex being breaking down as warmer air penetrates from further south (via the north Atlantic jetstream presumably). The following week, they confirmed it had happened. Air was sinking from the stratosphere into the lower atmosphere (troposphere) over the Arctic towards the surface. This subsequently affected the north Atlantic jetstream, slowing it down, prompting it to loop and diverge, even reverse from west to east. That, in turn has affected winds nearer the surface over Britain and Europe. The intense anticyclone built over Scandinavia had a central pressure of 1056 millibars on 28th, but was forecast to decrease rapidly over the next few days. As the polar vortex broke down, warmer air flowed towards the North Pole, in constant darkness at this time of year, the temperature there nudging above freezing at one point, if I remember reading rightly. Certainly temperatures in parts of Siberia have been 35oC above the historical average this February, and a record 61 hours above freezing in Greenland so far this year (The Guardian). 

Links
Weather
UK Met. Office website


https://www.metoffice.gov.uk/guide/weather/symbols
Meteo France - http://www.meteofrance.com/accueil
Meteoalarm (Europe) – weather warnings across Europe, with links to national weather services -  https://www.meteoalarm.eu/
Met. Office News Releases
UK Weather stats (rainfall, temperatures, sunshine hours) for January (01/02/18) - https://www.metoffice.gov.uk/news/releases/2018/january-statistics
February new releases point to a trend to generally drier and much colder weather, especially at the end of the month, and into March, thanks to warming of the stratosphere over the Arctic triggering a slowing of the north Atlantic jetstream and an intense anticyclone building over Scandinavia bringing very dry and bitterly cold northeasterlies from Siberia.
How long will the cold conditions last? (09/02/18) – mention of sudden stratospheric warming possibility prompting marked changes lower in the atmosphere (in the troposphere) to the course of the jetstream and synoptic pattern. https://www.metoffice.gov.uk/news/releases/2018/how-long-will-the-cold-conditions-remain
A mixed week of weather (12th February) – some milder and wetter weather, but confirmation that stratospheric warming over the Arctic has occurred, which could shape subsequent weather - https://www.metoffice.gov.uk/news/releases/2018/a-mixed-week-of-weather-ahead
Freezing conditions to last into spring (March) (23/02/18) – blocking pattern setting in as high pressure settles and intensifies over Scandinavia, winds shift to easterly / north easterly, bringing in bitterly cold air from Siberia. https://www.metoffice.gov.uk/news/releases/2018/freezing-start-to-spring
Bitterly cold with widespread snow (25th February) – the coldest weather of winter 2017/18 so far, and the coldest since 2013, when bitterly cold easterlies set in during the first half of March and persisted until May. No word yet, though as to when this year’s blocked, cold pattern will break.
https://www.metoffice.gov.uk/news/releases/2018/cold-and-snowy-week-ahead
Bitterly cold with snow (27/02/18) – amber and yellow weather warnings around the UK this week (26Feb – 2nd March), bitter cold, especially with wind chill; and snow in the east and southeast on Tuesday. March to begin with the possibility of snow, ice in southern England as fronts come in from the south as low pressure passes over Iberia (Storm Emma, according to the Portuguese weather service).
https://www.metoffice.gov.uk/news/releases/2018/bitterly-cold-weather-continues
Meteo France News Releases
An exceptionally mild but perturbed January with a succession of named storms - http://www.meteofrance.fr/actualites/58919551-janvier-2018-mois-de-tous-les-records
Tempête David affects northern France (and the UK) (18/02/18) - http://www.meteofrance.fr/actualites/58131340-tempete-david-sur-le-nord
http://www.meteofrance.fr/actualites/57448719-retour-sur-la-tempete-eleanor-des-2-et-3-janvier
Snowy and cold start to February - http://www.meteofrance.fr/actualites/59115031-debut-fevrier-froid-et-neigeux . Subsequent snowy episodes during the first week of February.

Shows the cold air forecast to come in from Russia / the NE
BBC News
Snow / weather disruption – BBC, 27/02/18 http://www.bbc.co.uk/news/uk-43207709
Water
CEH hydrology / monthly hydrological summaries for the UK
Environment Agency – River and Sea Levels, England
Environment Agency – Weekly and monthly water situation reports
Similar info’ for Scotland and Wales, at respectively, SEPA and Cymru
Eaufrance
Vigicrues (flood warnings and gauged river flows, France) - https://www.vigicrues.gouv.fr/
Other
The Guardian – online 27/02/18, paper edition 28/02/18:

River Lavant Revival after Longtime-no-see

River Lavant February 2018

Saturday, January 6, 2018

New Year, New Tidal Troubles along the Hamble River

Near the Hamble mouth at high tide, 3rd January
The photos here are from my walk to Warsash during the very high tide around 11.30am on Wednesday 3rd January; mainly along the lower Hamble near where it enters Southampton Water. 

2nd January 2018, the early hours: the first of two full moons this month. This one informally known as the Wolf Moon. It was a also a "supermoon", being full at perigee (its closest point to the Earth in its orbit around the Earth). Though the ensuing spring tides around Britain weren't forecast to be as high of some of those we have seen in recent years, they were raised through a combination of low atmospheric pressure and strong ( sometimes gale force) onshore winds. They came as a succession of low pressure systems crossed the British Isles; the jetstream being over the British Isles in the first week of January. One of these lows was so-called Storm Eleanor (but all the Eleanors I know aren't at all stormy) which passed over the British Isles on Wednesday 3rd January. It had a central pressure of 966 millibars at one point, centred over southern Scotland / the far north of England. Tidal surges of around 30cm above the astronomical forecast heights along the south coast on Wednesday and about 46cm on Thursday. These took the height of first high water at Southampton and Warsash to 5.14m on Wednesday and 5.24m on Thursday; triggering the EA to issue a flood alert.

Flooded path and bank erosion near the Hamble mouth
On Tuesday evening and Wednesday morning, there were more than sixty flood warnings and well over a hundred flood alerts. Some of them included river (fluvial) flooding because of rivers rising in response to the rain since Boxing Day (mostly East Anglia and the Midlands). Most of them, though were coastal and estuary; mainly western and southern coasts of England. There were warnings along the tidal Wye and Severn; though as there were no severe flood warnings here, it didn't sound as bad as it did during the high spring tides / tidal flooding this time four years ago. Over the course of Wednesday, the flood count went down; but Storm Eleanor also affected western continental Europe particularly France and Germany. In France, the Vigicrues river map was turning yellow with touches of orange as rivers rose after heavy rain and (in mountainous areas snow); and, as on this side of the Channel, the effect of strong winds and high tides along the Channel and Atlantic coasts. There were flood alerts along all the major rivers and their tributaries - plus ca change (see notes last month mentioning the Loire stuck at estival levels). There was a vigilance orange along the Lower Seine because of a triple whammy of strong winds generating waves; high tides; and the high volume of water flowing downstream, thanks to most of its main tributaries running high for sometime. By Friday evening, the flow through Paris had reached 1000 cubic metres per second (over 1100 cumecs on Monday 8th). Even after the tides waned and the weather became drier from the following weekend (6th / 7th) the larger rivers were still rising as the heightened flows from the tributaries propagated downstream. At Saumur, the Loire was forecast to peak at around 3000 cumecs on Tuesday 9th January (a month earlier it had only just made it to 200 cumecs).

On the Wednesday - windy but sunny after several days of rain during the middle of the day - I went down to Warsash. It was very windy, but bright along the shore. Southampton Water was very choppy and tide was rising on the foreshore, with about 45 minutes to go before first high water. The waves were about 50cm high and much smaller than they would have been in the open sea. I was able to walk along the shore; the backshore widening heading towards the Hamble.


The trouble came, though when I tried walking up the Hamble from the shore (see photos above). The path along the raised bank was flooding as waves splashed over the low wall separating it from the Hamble. It was also flooding beneath the bank, at the far end of the lagoon. I tried both, but didn't get far. I got as far as the gate; clambered over it and clamber back over it again; going any further clearly a lost cause. With the tide remaining high through the middle of the day (HW2 14:05h), I had no choice but to walk back along the shore to the path up to Cowes Lane; then double back along Hook Park Road to get to Warsash and the Quay. I got to the quay about half-twelve; about an hour after HW1. Though no water in the quay car park now, it was clear from the seaweed debris that it had been. By now, the path up the Hamble past the Pink Ferry was walkable; but had large puddles which had been there for a while because of the rain. They were there when we'd walked this way New Year's Day afternoon.

On the Thursday, the tide was even higher. I didn't go down there; but over the next few days numerous photos and videos appeared on Facebook with flooding on both sides of the Hamble, all along it, including Warsash, the Bunny Meadows path, the shore at Lower Swanwick. On the west side, it had spilled along the road behind Hamble Quay (a few motorists unwisely trying to negociate it). Among the footage on the Warsash side was a video posted by Warsash Harbour Master. This showed water spilling both into the car park (a number of cars and vans parked there - time they put up signs warning people) and into the sailing club / marina nextdoor; though unlike cars, boats float. This was the highest tide in this suite of spring tides; and probably one of the highest since 2014.

The tidal cycle subsequently waned with the moon, with drier and much colder weather coming in over the weekend 6th / 7th January.


Links / sources of information:
UK Met. Office - https://www.metoffice.gov.uk/
          
Environment Agency (England):

France
Météo France – forecasts and weather news, weather warnings
http://www.meteofrance.com/accueil
Vigicrues (flood warnings, links to gauging stations with real-time river levels and flows: https://www.vigicrues.gouv.fr/

Monday, December 18, 2017

Musings and Ousings Around York - Part Two

York floods 1982 - 2015

Flood heights near Ouse Bridge


Below: Flood heights at Ouse Bridge (gardens between Ouse Bridge and Skeldergate Bridge) – given in feet and inches. Most recent, and the highest 2000.









Date
Height / m
Height /ft
Comment
04/11/2000
5.4
17’8”

1636
5.3
17’ 6”

27/12/2015
5.2
17’1”

26/09/2012
5.07
16’8”

1831
5.08
16’8”

05/01/1982
5.05
16’7”

March 1947
4.99
16’ 4 ½ “

1763
4.94
16’ 2 ½ “

December 1978
4.85
15’ 11”

1892
4.77
15’8”

1991 (Feb?)
4.72
15’6”

1995 (Jan?)
4.70
15’5”


The floods of 2012 and 2015 have yet to be added to the Skeldergate gauge; and I didn’t notice them marked anywhere else either. Regardless or real estate value and the property market, they shouldn’t hide these things; though may be have information near the gauge / floodmark about flood defences reducing the risk.

The 1982 flood was the first one I remember hearing about clearly; as a 14 year old deeply into rivers. December had been cold with heavy falls of snow throughout Britain, which thawed rapidly as it turned mild and wet. Around new year, there was flooding on the River Severn. Then the highs shifted to Yorkshire; the Wharfe bursting its banks; Dad noting this having painted it in much more benign conditions at Bolton Abbey the summer before. In York there was widespread flooding around the city; and on the tidal Ouse at Cawood and Selby downstream. I recall hearing about it all on the BBC evening TV news; and on John Craven’s Newsround. Also stuck cuttings from The Guardian into my diary; one showing a bleak picture of the flooded Vale of York somewhere around Selby. All the bleaker as, though the weather was better back home, I was at the difficult age of 14; unhappy and anxious; spotty and overweight; I wanted friends at school but couldn’t find anyone on my wavelength; but realistically, my frequency was someway off the conventional spectrum expected at that age. The news reports of floods focused on Britain; but there was also widespread flooding in Europe (presumably through a similar combo or melting heavy snowfalls and heavy rain coinciding); including the Seine in Paris; and Vistula in Poland. The BBC News mentioned the latter, Poland being in the news anyway because of martial law being imposed by the communist block  General Yarozelski just before Xmas 1981.
I don’t know about Scotland, but I’m pretty sure January 1982 flooding episode in England & Wales where melting of heavy snowfall was a big factor. Since then all the major floods in England and Wales have been  pluvial (rainfall). Relatively mild winters (eg 2015/16, 2000/01). During the colder winters (early 1991, 2009/10, 2010/11) the snow has been less heavy, shorter lasting and thawed slowly. The last two cold spells were largely cold and dry.
The 1982 York flood prompted the building of flood defences later in the 1980s, including floodgates outside the row of houses alongside the river above Scarborugh railway bridge; the Clifton Ings floodwall / sluices; floodbank alongside playing field below Clifton Bridge; and the Foss Barrier.


Foss flood barrier, operating since 1988

1991 – January or February – the biggest flood in York since 1982; as far as I’m aware the flood defences coped and it was just mentioned in passing by The Guardian with a photo. The first I heard of it was there and not on TV / radio. This came during an otherwise prolonged relatively dry period; with a succession of drier than average winters straining groundwater and chalk streams in southern England.
November 2000 – the highest flood recorded here. On the night of the flood (3rd November), it was touch and go whether all the flood defences would hold in the rising water; predicted levels raised after further heavy rain on the Pennines. This was one of the notorious areas during a period of prolonged, repeated widespread flooding across the UK. For several months that autumn, one low pressure moved in after another; some of them slow moving, leading to heavy rainfall accumulations. The floody trouble began in southern England in October, affecting SE England, including Lewes on the Sussex Ouse. Then on the night of Sunday 29th October there was a storm and strong winds. We had a power cut lasting several hours in Church Crookham, Hampshire, the winds bringing down trees and branches over power lines. The power was restored in early hours of Monday; but several more shorter power cuts for about a year afterwards everytime the wind got up. However, we got off lightly; something which became clear the following day amid news reports of rivers rising across the country. Among the first to rise were the reactive Wealden (the Mole) and Pennine rivers; then the slower respoinding ones like the Severn. The Severn floods were among the worst since 1947 and strengthened calls for better flood defences along the middle Severn through Shropshire and Worcestershire. In the north, meanwhile, reporters in wellies in York. I thought I heard one BBC Radio 4 news report mentioning the Aire charging through Leeds with a flow in excess of 1000m3s-1. The Aire flows into the Ouse downstream, so it didn’t contribute to the flooding in York; but the Vale of York was badly affected for sometime afterwards. For the remainder of 2000, there were repeated flood warnings here; and there was a further (but lesser) flood in January 2001. The spring and summer of 2000 had been wet, too: the Ouse flooded in early June. The EA used that flood as a test of their revamped flood warning service, ie flood alert, flood warning, severe flood warning. News crues’ floody reports reminded me another visit to York and the Ouse was overdue. I made two trips there during the much calmer autumn and winter of 2001. The first one, in late September was solo; with a couple of nights at YHA York and a day looking round before an OU revision weekend at the University of York. During my wanderings, I some verse to the tune of The Grand Old Duke of York nursery rhyme flowed into mind. Verses added as more floods happened.

Oh the dark brown Ouse of York
In its 2000 flood
Rose over the top of the bank
And caked the place in mud
And when it was up it was up
And when it was down it was down
And when it was only half way up
It was neither up nor down.

Then at the beginning of December, a duo trip, again based at the YHA, arriving on Saturday 1st December to view Treske furnishings in Thirsk.  We also had a look round York and walked along the river. I remember particularly the Millennium Bridge and golden reflections of Ouse Bridge in bright winter sunshine. In complete contrast to the winter before, and no doubt a relief to people living and working in the area, it was a largely dry anticyclonic winter; though there was minor flooding in February 2002. It had also been a fine, bright autumn, with the autumn colours lingering into early December.

26th September 2012
Unusual timing: September is usually dry, the weather breaking much later in the autumn, if it’s going to. 2012, though had been a very unusual year: starting off dry with real worries about drought in large parts of England and Wales after two successive dry winters. Then, an about-turn in April with heavy rain from the middle month. The Severn and Ouse flooded during the last week. Even more unusually, the groundwater and southern chalk streams recharged; rain percolating through the soil when it would normally evaporate or be taken up by plants. The early summer was wet, too. A lull later in the summer; but then it all started up again in late September. There was so much rain over Yorkshire that the Ouse rose to its highest level since the 2000 flood; though as far as I know the flood defences held limiting property flooding. News of this flood (mainly online) incidentally, distracted me briefly from a renewed period of health-related preoccupation and anxieties post-ITP diagnosis. While walking along the Swale at Richmond the year before, I thought York was about due for another large flood; to which the Swale would surely contribute. Through my life, they’d tended to happen about every ten years; though purely a perception and not a fact. After this flood, then, I thought the Ouse had had its fill for a while. But I was wrong…

 Pages from my scrapbook, December 2015


Storm Eva December 2015 – Yet another when one rain-bearing low pressure after another rammed the country leading to widespread flooding. Two winters before, (2013/14) it had been the south and Midlands. Now it was the north’s turn; and the low pressures had names (adopted by the Met.Office from an alphabetical list of names chosen by the public). Most notoriously, Storm Desmond 5th/6th December causing unprecedented, devastating flooding throughout Cumbria and to a lesser degree the Pennines. Come Christmas, warnings of another low developing, this one called Eva, set to hit on Boxing Day. At first they thought Cumbria would spare the brunt yet again; but this time the biggest problems were in Yorkshire, including York. The Ouse exceeded its 2012 level, but was some way below that attained in 2000. However, the property flooding was widespread throughout the city. Much of it was due to the failure of the Foss flood barrier, or more precisely, the Environment Agency – after considerable and careful thought – lifted the barrier to prevent the control room flooding. Normally, when the barrier is closed, it prevents the rising River Ouse backing up the River Foss and flooding the centre of city; pumps, meanwhile discharging the flow from the Foss into the Ouse near the barrier. When we visited York at the beginning of December 2017, construction work was in progress by the barrier installing eight new higher capacity pumps and a new control room which is less likely to flood. There as also major flooding on the River Wharfe which joins the tidal Ouse at Cawood above Selby. At Tadcaster it took out (destroyed) a historic stone bridge, which didn’t reopen until more than a year later. At Flint Mill Weir, near Tadcaster, the CEH / NRFA say the peak flow was around 500m3s-1 for a catchment size of 758km2 and mean flow of around 18m3s-1


 Foss flood barrier construction work, December 2017


The Vale of York is very flat and was a lake during the last ice age;  the Ouse and Humber only appearing when the ice melted and the lake drained away. 
Finally the naming of rivers, the Ure-Ouse and Humber are one river; and one of the longest in England; though I guess you could take the Ure-Ouse to be a tributary of the Trent, meeting the Trent at Trent Falls. I don't know why names change along this river system and not others. Maybe it's the marked change in the character and landscape reflecting local Geology moving east from hilly limestone dales to the flat Vale of York, then wide estuary. One theory says the  Ure (Yore) and Ouse sound similar and have the same derivation, probably water as most British river names do. Others say it’s the Ouse Gill Beck, flowing in below the confluence of the Ure and Swale which usurps the title. Broadhead says the Ouse (this stream) was Born in a Workhouse.

Books and Websites
Books

Richard Bell – Yorkshire Rock – A Journey through Time, Earthwise (2006) – geology across Yorkshire, early Mesozoic era to Quartenary.

Ivan E. Broadhead - Portrait of the Yorkshire Ouse, Hale (1982) – bought secondhand in about 1983. Even after all this time, still a good read and appreciation of the river.

Websites

York Stories – Why does York flood?http://yorkstories.co.uk/why-does-york-flood/
Flood Heights on the Ouse | York Civic Trust

River Foss Barrier - Wikipedia

York's Foss flood barrier: New pump to be installed - BBC News

Pre-Christmas Water Status Update

Water Status Reports – A Tale of Contrasting Flows


Thornton-le-Dale flow gauge in snow 30/11/17

Apart from the heavy rains prompting flood warnings in the northern England during the third week, November was a largely a relatively dry month across the UK; especially in the English lowlands, southern and central Scotland. The autumn (1st September – 30th November) rainfall total was well down in these areas, too. In southern and SE England, rainfall deficits have been building for the past 12-18 months; reflected in low groundwater and river levels and low river levels in these areas. A growing number of rivers across southern England are running well below normal: the Thames among them; with the Great Stour in Kent and the Lee in Hertfordshire exceptionally low; and hitting new record lows for November.
Great Stour, Canterbury, August 2014
The Stour gauge is just upstream Canterbury (Horton), where it is a chalkstream fed by groundwater percolating through the North Downs. The CEH and EA hydrographs show it has been running well below normal for at least the past twelve months; with no increase in flow since the summer. On 16th December, the River Lavant above and through Chichester, West Sussex was still dry. I have not seen any water in the river for the past eighteen months.Most chalk wells in southern England have yet to recharge and one in Kent (Little Bucket Farm) is dry according to CEH. Though most reservoirs are at least 80% capacity; some in the south are well below that, especially Bewl in Kent which was only 33% capacity at the end of November. The watery outlook for next year is dependent on how much rain falls over the winter and early spring. To bring the low level rivers and wells back into the normal range for the time of year will take “appreciably above average” rainfall, say CEH. If it doesn’t happen and we have, for the second year running,  another dry, anticyclone-dominated winter, this could strain water resources and lead to environmental stress by next summer.

Dry stream bed at Mid Lavant, 16/12/17

The same location in February 2013, after a wet winter
 Still Missing - River Lavant, West Dean 16/12/17

It has also been very dry in France / western Europe for much of this year, with similarly low, or even lower river flows and groundwater levels; due to high pressure over the continent to the west in the Atlantic keeping the rain away. The drought has been particularly pronounced in the south, where there were forest fires in the summer; and the wine harvest has been poor due to a combo’ of a spring frosts and summer heat. Even at the end the of November, the rainfall deficit was still 40% in some areas; and the Loire, the longest river in France with total catchment area of over 100,000km2 was still running below 200m3s-1 (Saumur, basin size here around 81000 sqkm). That’s about what they’d expected here in summer, ie estival.  Things began to change in late November when the synoptic pattern finally shifted; though more for the benefit of the east of the country than the west and Loire valley.

The Derwent-Cocker confluence, Cockermouth 25/09/17
As in November 2016, the corresponding monthly rainfall totals were very influenced by heavy rainfall falling over one or two days: most notably this year, November 22nd, when heavy rain fell in NE England and the Scottish borders affecting the Lake District, Pennines and River Tweed. During that week, the EA had a number of flood warnings out in these areas, including on the rivers I have visited this year and last: the Tweed, the Greta at Keswick and the Eden. The CEH say that  the Lune and Eden hit record high peak flows for the month of November in records going back to the 1960s; the Eden apparently exceeding its flow at the height of the November 2009 Cumbrian floods.

Eden-Caldew confluence, Carlisle, September 2016
According to the NRFA, the peak flow at Sheepmount (Carlisle) during that episode was over 1000m3s-1. However, there’s no mention of any flow figures in the November hydrological reports. The CEH November monthly hydrological summary shows a hydrograph for the Eden at Temple  Sowerby, indicating a flow of about 300m3s-1. The NRFA gives a peak flow at Temple Sowerby, 18/11/09 was just under 350m3s-1; but that figure is not exceptional in the record for that gauging station, going back to 1964. The highest recorded peak flow there was over 900m3s-1, 08/01/05, which stands out among the other readings in the data table like a sore thumb. The catchment here is around 600km2 and is upstream from everything flowing in from the Lake District via the Eamont and Caldew and far north Pennines. The Sheepmount gauge is just downstream of the Caldew confluence in Carlisle, therefore takes in the whole catchment (2287km2); though the EA is still giving near real-time river levels here, the NRFA say that during the big Storm Desmond flood, the channels shifted, meaning readings at the gauge are no longer comparable with previous ones dating back to 1968. During this year’s episode, the Swale, which rises close to the Eden, also ran high; discharging into the Ure-Ouse upstream of York. At the end of that week (24th November), the Ouse spilled onto the quays in York: when we visited it the following week, they were hosing away the mud.

Thornton-le-Dale in snow 30/11/17
After this soggy interlude, the weather pattern shifted, with high pressure extending all the way up the north Atlantic, diverting the lows up and over the British Isles and down over Scandinavia and the North Sea. This brought rain to eastern France, raising the River Seine to comfortably normal levels. The airflow, though was northerly, bringing chilly weather to Britain, with some snow. During the last week of November, it got very wintery over NE England: we know this as we were away that week in Thornton-le-Dale, in the Vale of Pickering. On Monday 27th, a bitterly cold northerly on the north facing coast at Whitby. The Wednesday, 29th, was a thoroughly miserable day in Thornton, with bitter cold, heavy rain and hail. Though the Pennine rivers had fallen, there were now flood alerts on rivers flowing off the North York Moors: the Esk and Derwent. A small rise (about 10cm) on the placid, steadily flowing Thornton Beck. Overnight the rain turned to snow. It continued snowing on the Thursday morning. A snowy walk along the Thornton Dale, followed by filling pie pub lunch at The Buck Inn. The rest of the week remained cold, with snow lingering in Thornton on Friday 1st December – likewise an ungritted Park & Ride car park on the east side of York. Snow still lingered on the North York Moors (which go up to about 300m) during the drive (road clear) to Whitby on the Saturday. Unusually during this snowy episode, the precipitation was coming in from the east, troughs in the North Sea and was mainly confined to the NE coast / far east of Yorkshire. Dry over the Pennines and NW England (which we wanted to avoid for a winter week away after Storm Desmond).

River Ouse, York, 1st December 2017
During the second week of December, it was the turn of the Midlands to get the snow (10th December. Icy in other areas, including the south on Monday 11th. This came shortly after the third named storm of the season, Caroline, which affected the far north of Scotland with strong winds. Monday 11th in southern England was wet and windy. In France, it was even windier, with gusts upto 160km/h on the west coast, according to Météo France. At Blois, on the Loire above Tours, there was a 121km/h gust, the third strongest since the station opened in 1990. Thanks to this rain, the Loire finally began to rise slowly from its estival levels; but still couldn’t quite make it to 500m3s-1 at Saumur. Often in winter there, the flow is in four figures. The Seine (Paris Austerlitz exceeded that figure on 12th and 15th December, with yellow flood alerts on some its tributaries, including the Marne, its largest.
One hopeful thing, maybe for the drier areas is, though high pressure never seems to be far away from western continental Europe, the December synoptic pattern so far is less blocked and much less anticyclonic than it was last year. Rainfall during November has wetted the soils, enabling further rain to percolate though the soil down to aquifers.

Links / sources of information:
UK Met. Office - https://www.metoffice.gov.uk/
          Weather news  releases - https://www.metoffice.gov.uk/news/releases
Met.Office (news release 01/12/17) – November and Autumn weather statistics
Environment Agency (England):
National and regional water situation reports, issued weekly and monthlyhttps://www.gov.uk/government/collections/water-situation-reports-for-england
River and Sea Levels
https://flood-warning-information.service.gov.uk/river-and-sea-levels
Flood warnings - https://flood-warning-information.service.gov.uk/warnings
Centre for Ecology and Hydrology (CEH), UK
Monthly hydrological summaries - https://nrfa.ceh.ac.uk/monthly-hydrological-summary-uk
Hydrological outlook - http://www.hydoutuk.net/latest-outlook/
National River Flow Archive – river flow data measured by gauging stations around the UK
https://nrfa.ceh.ac.uk/data/search
CEH Drought Portal - maps of dryness around the UK for the past month - 24 months. Data back to 1961
France
Météo France – forecasts and weather news, weather warnings
http://www.meteofrance.com/accueil
Vigicrues (flood warnings, links to gauging stations with real-time river levels and flows:
https://www.vigicrues.gouv.fr/
Eaufrance – national monthly hydrological reports - http://www.eaufrance.fr/

Other water news
English rivers polluted by powerful insecticides, first tests reveal | Environment | The Guardian 13/12/17
Sampling was on twenty-three rivers around the UK, mainly in England and Wales. The Eden and Twyi (Wales) and three other rivers were in the clear; but neonicotinoid insecticides were detected in all the others. The River Test, a prime angling river in Hampshire was among them; as were the Yorkshire Ouse and the Teme. Levels were particularly high / bad in the Waveney and Great Ouse in East Anglia and the Tame in the Midlands.
CEH news – Mapping ephemeral / intermittent rivers and streams across the UK and Europe. The Lavant in West Sussex is among them.
https://nrfa.ceh.ac.uk/news-and-media/news/mapping-intermittent-rivers-and-ephemeral-streams-across-europe