WW2 D-Day Weather

 In the late spring of 1944, most people knew the invasion of mainland Europe was imminent, but very few knew where and when. It was the job of the senior meteorologists to advise the Supreme Commander as to when.

Bomber and fighter aircraft each required different cloud conditions.
Very strict minimum weather conditions were laid down, with different flight criteria for each arm of the operation. Bomber and fighter aircraft each required different cloud conditions. Gliders needed a moonlit night with no fog or mist.

The Army needed firm dry ground, so no heavy rain before the date. The Navy needed winds no stronger than 10 knots, good visibility and no prolonged high winds in the western approaches for the days immediately preceding the operation, thus limiting the size of any waves and swell in the English Channel. These quiet conditions should then persist for as long as possible after the initial assault.

It would have been much easier if the date of the assault could be decided at very short notice, but this was not possible, as a large invasion force could not be kept waiting around indefinitely for suitable weather.

It was decided that the senior meteorologists of the Meteorological Office, the Naval Meteorological Service and the Weather Service of the United States Army Air Force, would work independently on predicting the likely weather patterns. Dr Stagg of the British Meteorological Office, seconded as a Group Captain in the RAF, was appointed as the co-ordinating forecaster to brief the Supreme Commander and his staff.

The forecasters were concerned with two parts of the forecast – the detailed requirements for the start of the invasion, and the much longer period for the build-up of the troops after that.

At first the meteorologists studied the climatology at the most likely time of the invasion, to give them an idea of the most usual weather for that time of year. This showed that either May or June was probably better than July, but it was already too late for arrangements to be made for May.

The tide, state of the moon and time of sunrise combined favourably on June 3rd and the following two days. A fine quiet spell in late May gave way to more unsettled westerly winds, and by the beginning of June there was a very common weather picture, with an Azores high pressure belt extending into the Bay of Biscay and a frontal system and its attendant low pressure areas stretching from Scotland and into the western Atlantic.

All the forecasting advice now hinged on the movement of the lows and the weather fronts, but in 1944 forecasters trying to see 48 hours ahead was at or beyond the limits of what was possible.

On the strength of this uncertainty on June 3rd, the Supreme Commander postponed the invasion…
It looked as though the weather in the Channel would be marginal for the proposed landings on June 5th. Being sandwiched between the high pressure belt over France and the low pressure further north meant that the south-westerly winds would be too strong and bring in too much cloud, making the bombing in advance of the attack very difficult. On the strength of this uncertainty on June 3rd, the Supreme Commander postponed the invasion for 24 hours.

The three weather centres continued to debate the possible solutions in the weather scenario. Low pressures were developing in the western Atlantic and moving northeast across Scotland. This kept the weather fronts to the northwest and consequently continued to feed in strong south-westerly winds through the English Channel.

The general consensus was that there was likely to be little change in the overall picture, but then unexpected developments occurred on Sunday, June 4th.

Although pressure was falling quickly over Ireland and a cold front was moving quickly east, an observation was being reported from a ship stationed due south of Iceland, which showed sustained, rising pressure. This observation was from a Royal Navy vessel stationed there for the specific purpose of providing meteorological observations from an area, which has a major influence on Britain’s weather patterns.

Stagg realised that nothing could stop the cold front moving through the Channel, and it now also looked as if a low pressure system out in the mid-Atlantic would slow down and intensify. More important, however, was the information from the Navy ship.

Taken together with all the other data, it could indicate that a ridge of high pressure was developing behind the cold front, which was presently sweeping over the Channel. If this continued, there could be enough of a window in the unsettled weather over the Channel, and the assault area, just for the critical hours on Tuesday June 6th.

If this happened, there could be a period of improved weather in the landing zones long enough to allow the first critical assaults to be made on June 6th. By the early hours of that morning, the weather would be suitable for the heavy bombers, although large areas of cloud might curtail later operations. This however, was likely to be high enough to enable the fall of shot to be spotted for the naval heavy guns.

Stagg now had to persuade the Supreme Commander to take advantage of this most unlikely break in the very unseasonable weather and hope that the German forecasters on the French coasts had not spotted this subtle change in the weather pattern.

…the weather outlooks had changed so violently in recent days.
Stagg informed General Bull on the Sunday evening of the probability of the weather window on the 6th (Tuesday), but it was treated with some understandable caution, since the weather outlooks had changed so violently in recent days.

On Sunday evening (June 4th), the Commanders-in-Chief and their senior staff assembled in the library. Stagg and Yates entered and briefed them on the recent weather developments, describing the latest optimism. Air Chief Marshal Tedder asked what confidence Stagg had in the forecast he had just given, and was told that the confidence was high for a spell of fine weather behind that cold front, but not so high for a continued settled spell after that.

The Supreme Commander then discussed the position with his Chiefs. The atmosphere was tense and grave. He then asked General Montgomery if there was any reason why they should not launch the attack on June 6th, to which Montgomery replied, “No. I would say go”

They all met again at 0415 on Monday, June 5th. The room was quiet when General Eisenhower asked Stagg for his opinion, and was told that no substantial change had taken place since the last briefing and that fair weather would extend through all of southern England that night and last into Tuesday afternoon.

There would be small amounts of cloud and the winds in the assault area would be Beaufort Force 3 to 4, locally Force 5. Later on Tuesday it would become cloudier with more unsettled weather at times again between Wednesday and Friday. The relief was immediate. The Supreme Commander broke into a broad smile and told Stagg that if this forecast came off they would all have a celebration when the time came.

Battle of Trafalgar

21st October 1805

HMS IMPLACABLE (ex Duguay-Trouin)

By Patrick Stacey

 Not many people know that a wooden walled battleship that fought in the Battle of Trafalgar was still afloat in 1949, some 144 years after the event.

 No!   Not Admiral Lord Nelson’s flag ship H.M.S. Victory, as she was already in dry dock and restored to her former glory.

 The ship I am referring to, and had a personal interest in, is a French 74-gun ‘man of war’ Duguay-Trouin. Built in Roquefort, France in 1801 she had a waterline length of 55m and breadth of 15m. Complement of 670 menUnder the command of Claude Touffet she survived the Battle of Trafalgar after causing severe damage to the British fleet.

 However, 14 days later she was sighted by Sir Richard Strachan’s fleet. In the ensuing engagement Claude Touffet and all his officers were killed.

 A prize crew was put on board the French ship and sailed back to England for a refit and then commissioned as H.M.S. Implacable. She saw service with the Mediterranean fleet until 1855 when she became a Royal Naval training ship.

 In the 1930’s the Royal Navy gave permission for HMS Implacable to be used as a private training ship in Portsmouth Harbour for Merchant Service cadets

 After the war the old ‘man of war’ became too costly to maintain and on December 2nd 1949 a tug took her in tow and she was scuttled off the Isle of Wight in the English Channel. The last ship afloat from the time of Trafalgar had been put to rest after 148 years.

St Swithin’s Day – July 15

 ‘St Swithin’s day if thou dost rain

‘For forty days it will remain

‘St Swithin’s day if thou be fair

‘For forty days ‘twill rain nae mair

 This is one of the several days from which, in folklore, the weather for a subsequent period is dictated. In popular belief, if it rains on St. Swithin’s Day, it will rain for 40 days, but, if it is fair, 40 days of fair weather will follow. St. Swithin was bishop of Winchester from 852 to 862. At his request he was buried in the churchyard, where rain and the steps of passers-by might fall on his grave. According to legend, after his body was moved inside the cathedral on July 15, 971, a great storm ensued.

Weather frequently changes around midsummer, and thus the tradition that this day influences the weather may stem from ancient pagan belief. On the European continent similar beliefs are attached to other saints (e.g.St, MÉDARD June 8, France).

However, according to the UK met Office, this ‘old wives tale’ is nothing other than a myth. It has been put to the test on 55 occasions, when it has been wet on St Swithin’s Day and 40 days of rain did not follow.

1994 Queens’s Birthday Storm

This South Pacific storm formed between 1st and 4th June 1994, and while not unusual, it affected a large number of yachts on route between New Zealand and Tonga and led to New Zealand’s largest air/sea rescue operation. Six yachts were abandoned and their crews picked up and one with its crew of three was lost.

This was not the cyclone season and the storm that developed was never officially named as such. In any case it had no core of central warm air characteristic of cyclones and hardly reached gale force winds while it was in the tropics.

None the less, its effects in the subtropics were devastating.

On June 2nd, a slight kink in the isobars of the synoptic chart near Vanuatu was the only indicator of what was about to take place.

The low pressure system developed and started to move south. Of particular significance is the area of high pressure over New Zealand that brought in a supply of cold, low level air from the Antarctic. Cold air does not mix easily with warm and the effect of this inflow was to force the existing warm air upwards. An upper level system was active and withdrew rising air faster than the incoming cold stream was able to replace it. Barometric pressure of the surface was reduced still further as the system increased in size.

This phenomenon of cold air being drawn into a deepening low pressure system is sometimes known as meteorological ‘bomb’

Dust Blankets Sydney

The media headlines today bring to mind the Melbourne Dust Storm on 8th February 1983. This was when south-eastern Australia was coming out of one of the worst droughts since European settlement leaving behind very sparse vegetation cover and a great deal of dry exposed red dust in the Mallee region. Strong north-westerly winds moving ahead of a cold front whipped up the dust into a fast moving wall creating a dramatic sight as it towered above the Melbourne skyline.

In 1852 another notable dust storm occurred in the Melbourne area on Sunday 19th December when The Tmes in London reported ‘a man riding his horse on the outskirts of Melbourne was unable to see the ears of his horse due to the streaming volume of hot, stinging dust’.

March 16 – 22nd Yesteryears

 

1286

King Alexander III of Scotland died when he was blown off a cliff at Inverkeithing, Scotland by a violent easterly gale.

1925

The infamous Tri-State Tornado raced 219 miles across Missouri, Illinois and Indiana. to become the deadliest single tornado in U.S. history. The storm left 695 people dead, 2,027 injured and an estimated $17 million dollars in damage with 15,000 homes totally levelled.

1978

28 people were killed and 300 injured as a tornado touched down and stayed on the ground for over three miles in the northern suburbs of New Delhi, India

1990.

An intense hailstorm struck the Sydney region in Australia producing strong winds and heavy rain in a swathe from Camden to Narrabeen, causing extensive damage.  Hailstones were measured up to 3 inches in diameter.  The total insured damage was estimated at $314 million Australian dollars,

2006

Cyclone Larry, the most powerful storm to hit Australia in 3 decades, slammed onto the Australian coast south of Cairns in the town of Innisfail with estimated sustained winds of 115 mph with gusts to 150 mph devastating sugar and banana plantations and leaving thousands homeless.  Damage totalled a half billion dollars.  Miraculously, no lives were lost and no serious injuries were reported.  At one point, Category 5 Larry packed wind gusts to Category 5 strength of 180 mph.