Case Study Daybed Uk Weather

  • Hurricane Sandy

    New York and its history of storms

  • Floods and flooding

    Floods can be devastating — costing the lives of people and animals, as well as destroying crops, homes and businesses.

  • Hurricane Katrina

    At least 1,500 people were killed and around $300 billion worth of damage was caused when Hurricane Katrina hit the south-eastern part of the USA. Arriving in late August 2005 with winds of up to 127 mph, the storm caused widespread flooding.

  • Severe Winters

    The list below may look like something that would happen in the Arctic, but all of them happened in the UK during two particularly severe winters - in 1947 and 1963.

  • Boscastle Floods

    On 16 August 2004, a devastating flood swept through the small Cornish village of Boscastle.

  • July 2013 heat wave

    A heat wave affected most of the UK from 3 to 23 July 2013, making this the warmest and sunniest July for the UK as a whole since 2006, and the third warmest on record.

  • Widespread snow March 2013

    In March 2013 an active weather fronts moving in from the Atlantic brought heavy rain and flooding to south-western parts of the UK.

  • Widespread snow January 2013

    A snowy spell of weather affected most the UK from 14 to 26 January 2013.

  • 2012 - a wet year

    In 2012 the weather regularly made the news headlines and if you asked somebody to describe 2012 in a single word they would probably say "wet".

  • November 2012 flooding

    This case study focuses on one week in November when four periods of rainfall brought widespread flooding to many parts of the UK.

  • July flooding 2012

    Persistent rain brought flooding to many parts of the UK during the first weekend of July. The impacts were numerous, ranging from flooded transport networks to disrupted sporting events.

  • April 2012 - Wet and windy

    April 2012 was the wettest April in the UK as a whole since records began in 1910. Within the UK there were some marked regional variations across the UK. Much of the rainfall was focused on the south.

  • UK Snow 4 to 5 February 2012

    4 to 5 February 2012, after a cold and settled spell, a significant fall of snow affected central and eastern parts of the UK. Some parts experienced 10 to 15cm.

  • Indian summer 2011

    An Indian summer is a warm, calm spell in autumn, around the end of September to the middle of November. The phrase comes from America and refers to the Native American Indians.

  • UK Snow 2010

    Many parts of the UK experienced significant snow events from late November to early December 2010. This case-study focuses on the period 28 November to 2 December.

  • Hurricane Igor hits Bermuda (20 September 2010)

    A Met Office forecaster was working on secondment in Bermuda during hurricane Igor. Some thoughts were gathered from somebody who experienced it in person.

  • The Russian heatwave of summer 2010

    The UK may have had another uneventful summer in 2010 but much of the European continent experienced an extreme heat wave. This case study will focus on events in Russia specifically. Russia was badly effected through July and the first half of August.

  • Ottery St Mary Hailstorm October 2008

    During the early hours of 30 October 2008 the small East Devon town of Ottery St Mary experienced an extreme weather event in the form of an exceptional hailstorm.

  • A snowy day in Winter 2005

    Heavy snow stops traffic on main route through Cornwall.

  • The heatwave of 2003

    More than 20,000 people died after a record-breaking heatwave left Europe sweltering in August 2003. The period of extreme heat is thought to be the warmest for up to 500 years, and many European countries experienced their highest temperatures on record.

  • UK freezing rain - 23 to 24 January 1996

    Freezing rain is fairly rare in the UK. When it does occur the consequences can be devastating. This case study looks at an occurrence which affected Wales, SW England and the Midlands in January 1996.

  • The Great Storm of 1987

    A powerful storm ravaged many parts of the UK in the middle of October 1987.

  • The Great Smog of 1952

    A fog so thick and polluted it left thousands dead wreaked havoc on London in 1952. The smoke-like pollution was so toxic it was even reported to have choked cows to death in the fields. It was so thick it brought road, air and rail transport to a virtual standstill. This was certainly an event to remember, but not the first smog of its kind to hit the capital.

  • The Great Storm of 1987

    A powerful storm ravaged many parts of the UK in the middle of October 1987.

    With winds gusting at up to 100mph, there was massive devastation across the country and 18 people were killed. About 15 million trees were blown down. Many fell on to roads and railways, causing major transport delays. Others took down electricity and telephone lines, leaving thousands of homes without power for more than 24 hours.

    Buildings were damaged by winds or falling trees. Numerous small boats were wrecked or blown away, with one ship at Dover being blown over and a Channel ferry was blown ashore near Folkestone. While the storm took a human toll, claiming 18 lives in England, it is thought many more may have been hurt if the storm had hit during the day.

    The storm gathers

    Four or five days before the storm struck, forecasters predicted severe weather was on the way. As they got closer, however, weather prediction models started to give a less clear picture. Instead of stormy weather over a considerable part of the UK, the models suggested severe weather would pass to the south of England – only skimming the south coast.

    During the afternoon of 15 October, winds were very light over most parts of the UK and there was little to suggest what was to come. However, over the Bay of Biscay, a depression was developing. The first gale warnings for sea areas in the English Channel were issued at 6.30 a.m. on 15 October and were followed, four hours later, by warnings of severe gales.

    At 12 p.m. (midday) on 15 October, the depression that originated in the Bay of Biscay was centred near 46° N, 9° W and its depth was 970 mb. By 6 p.m., it had moved north-east to about 47° N, 6° W, and deepened to 964 mb.

    At 10.35 p.m. winds of Force 10 were forecast. By midnight, the depression was over the western English Channel, and its central pressure was 953 mb. At 1.35 a.m. on 16 October, warnings of Force 11 were issued. The depression moved rapidly north-east, filling a little as it went, reaching the Humber estuary at about 5.30 am, by which time its central pressure was 959 mb. Dramatic increases in temperature were associated with the passage of the storm’s warm front.

    Warning the public

    During the evening of 15 October, radio and TV forecasts mentioned strong winds but indicated heavy rain would be the main feature, rather than strong wind. By the time most people went to bed, exceptionally strong winds hadn’t been mentioned in national radio and TV weather broadcasts. Warnings of severe weather had been issued, however, to various agencies and emergency authorities, including the London Fire Brigade. Perhaps the most important warning was issued by the Met Office to the Ministry of Defence at 0135 UTC, 16 October. It warned that the anticipated consequences of the storm were such that civil authorities might need to call on assistance from the military.

    In south-east England, where the greatest damage occurred, gusts of 70 knots or more were recorded continually for three or four consecutive hours. During this time, the wind veered from southerly to south-westerly. To the north-west of this region, there were two maxima in gust speeds, separated by a period of lower wind speeds. During the first period, the wind direction was southerly. During the latter, it was south-westerly. Damage patterns in south-east England suggested that whirlwinds accompanied the storm. Local variations in the nature and extent of destruction were considerable.

    In pictures

    How the storm measured up

    Fig. 1 shows maximum gusts (in knots) during the storm.

    Comparisons of the October 1987 storm with previous severe storms were inevitable. Even the oldest residents of the worst affected areas couldn’t recall winds so strong, or destruction on so great a scale.

    • The highest wind speed reported was an estimated 119 knots (61 m/s) in a gust soon after midnight at Quimper coastguard station on the coast of Brittany (48° 02′ N 4° 44′ W).
    • The highest measured wind speed was a gust of 117 knots (60 m/s) at 12.30 am at Pointe du Roc (48° 51′ N, 1° 37′ W) near Granville, Normandy.
    • The strongest gust over the UK was 100 knots at Shoreham on the Sussex coast at 3.10 am, and gusts of more than 90 knots were recorded at several other coastal locations.
    • Even well inland, gusts exceeded 80 knots. The London Weather Centre recorded 82 knots at 2.50 am, and 86 knots was recorded at Gatwick Airport at 4.30 am (the authorities closed the airport).

    A hurricane or not?

    TV weather presenter Michael Fish will long be remembered for telling viewers there would be no hurricane on the evening before the storm struck. He was unlucky, however, as he was talking about a different storm system over the western part of the North Atlantic Ocean that day. This storm, he said, would not reach the British Isles — and it didn’t. It was the rapidly deepening depression from the Bay of Biscay which struck.
    This storm wasn’t officially a hurricane as it did not originate in the tropics — but it was certainly exceptional. In the Beaufort scale of wind force, Hurricane Force (Force 12) is defined as a wind of 64 knots or more, sustained over a period of at least 10 minutes. Gusts, which are comparatively short-lived (but cause a lot of destruction) are not taken into account. By this definition, Hurricane Force winds occurred locally but were not widespread.

    The highest hourly-mean speed recorded in the UK was 75 knots, at the Royal Sovereign Lighthouse. Winds reached Force 11 (56–63 knots) in many coastal regions of south-east England. Inland, however, their strength was considerably less. At the London Weather Centre, for example, the mean wind speed did not exceed 44 knots (Force 9). At Gatwick Airport, it never exceeded 34 knots (Force 8).

    The powerful winds experienced in the south of England during this storm are deemed a once in 200 year event — meaning they were so unusually strong you could only expect this to happen every two centuries. This storm was compared with one in 1703, also known as a ‘great storm’, and this could be justified. The storm of 1987 was remarkable for its ferocity, and affected much the same area of the UK as its 1703 counterpart.

    Northern Scotland is much closer to the main storm tracks of the Atlantic than south-east England. Storms as severe as October 1987 can be expected there far more frequently than once in 200 years. Over the Hebrides, Orkney and Shetland, winds as strong as those which blew across south-east England in October 1987 can be expected once every 30 to 40 years.

    The 1987 storm was also remarkable for the temperature changes that accompanied it. In a five-hour period, increases of more than 6 °C per hour were recorded at many places south of a line from Dorset to Norfolk.

    The aftermath

    Media reports accused the Met Office of failing to forecast the storm correctly. Repeatedly, they returned to the statement by Michael Fish that there would be no hurricane — which there hadn’t been. It did not matter that the Met Office forecasters had, for several days before the storm, been warning of severe weather. The Met Office had performed no worse than any other European forecasters when faced with this exceptional weather event.

    However, good was to come of this situation. Based on the findings of an internal Met Office enquiry, scrutinised by two independent assessors, various improvements were made. For example, observational coverage of the atmosphere over the ocean to the south and west of the UK was improved by increasing the quality and quantity of observations from ships, aircraft, buoys and satellites, while refinements were made to the computer models used in forecasting.

    Strength of gusts

    Fig 1. Graphic showing areas with strengths of maximum gusts.

    Web page reproduced with the kind permission of the Met Office

    Other MetLink resources linked to the 1987 storm:

    Weather articles:

    Damage to trees and woodlands in the storm of 15-16 October 1987, Quine, 1988
    The Storm of 15-16 October 1987: A personal experience, H.D.Lawes, 1988
    The Great Storm of 1987, Burt & Mansfield, 1988
    The storm, the Media and the Enquiry, J. Houghton, 1988

    Teachers TV – the Great Storm of 1987

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