The Royal Meteorological Society: How Britain Learned to Understand the Weather

The Royal Meteorological Society: How Britain Learned to Understand the Weather

Britain has always had weather. What it lacked, for a surprisingly long time, was an organised way of understanding it. Rain arrived, crops failed, ships disappeared and gentlemen peered anxiously at barometers. Afterwards, everyone discussed the matter at considerable length. This remains, in fairness, a recognisably British system.

By the middle of the nineteenth century, however, a group of scientists decided that talking about the weather should involve more than noting that it had turned rather unpleasant. On 3 April 1850, ten men gathered in the library of Hartwell House near Aylesbury, the home of the astronomer Dr John Lee. There they founded the British Meteorological Society.

Their stated purpose sounded wonderfully ambitious. They wanted to advance meteorological science by identifying the laws governing climate and atmospheric phenomena. In other words, they hoped to find order in something that appeared to specialise in ruining picnics without warning.

The founders included James Glaisher, an astronomer and pioneering balloonist who would later climb to dangerous altitudes to study the atmosphere. The Society also attracted Luke Howard, the man whose cloud classification system gave us names such as cirrus, cumulus and stratus. Before Howard, clouds were mostly described as fluffy, threatening or probably about to spoil the washing.

Interest grew quickly. By May 1850, the Society had around 90 members. This early enthusiasm reflected a wider Victorian appetite for measurement. Nineteenth-century Britain loved instruments, tables, classifications and scientific associations. If something existed, Victorians wanted to measure it, label it and discuss it over dinner.

Meteorology presented an awkward challenge. A scientist could examine a rock for as long as necessary, but the atmosphere refused to sit still. Weather crossed counties and national borders. A pressure reading from Buckinghamshire meant little without comparable observations from London, Edinburgh, Dublin or the Atlantic coast.

The Society therefore encouraged systematic observation. Members recorded temperature, rainfall, air pressure, wind direction and cloud conditions. More importantly, they worked towards common methods. A thermometer placed beside a sunny brick wall could produce a very impressive reading, but it would not tell anyone much about the actual air temperature.

Standardisation transformed scattered observations into usable science. Instruments needed consistent designs. Observers needed agreed procedures. Measurements had to take place at comparable times and under comparable conditions. The task sounded tedious because much of it was. Yet science often advances through disciplined boredom.

Britain already had weather observers before 1850, including enthusiastic landowners, doctors, clergymen, naval officers and amateur naturalists. The Society helped connect them. Their individual diaries and tables became part of a larger scientific conversation about storms, rainfall patterns, seasons and climate.

A common myth suggests that meteorology began when somebody invented the weather forecast. In reality, recording and forecasting developed as related but distinct activities. The Royal Meteorological Society promoted scientific knowledge, professional exchange and research. The Meteorological Office, founded under Robert FitzRoy in 1854, developed operational services for government, shipping and eventually the public.

FitzRoy understood that weather information could save lives. The Royal Charter Gale of October 1859 wrecked or damaged hundreds of ships around the British coast and killed many people. Using observations transmitted by telegraph, FitzRoy began issuing storm warnings. In 1861, he also launched Britain’s first public weather forecasts.

The forecasts attracted enormous attention and considerable mockery. Critics treated prediction as fortune-telling performed with barometers. When forecasts failed, newspapers complained. When they succeeded, people tended to forget that anyone had doubted them. The basic relationship between the public and meteorologists had already achieved its modern form.

Meanwhile, the Society gained institutional authority. It received a Royal Charter in 1866 and became the Meteorological Society. In 1883, it adopted the name Royal Meteorological Society. These changes represented more than Victorian fondness for impressive titles. A charter gave the organisation formal status and strengthened meteorology’s claim to recognition as a serious scientific discipline.

That recognition mattered because meteorology occupied an uncertain position. It borrowed from physics, mathematics, astronomy, geography and oceanography. Critics sometimes viewed it as a collection of observations rather than a coherent science. The Society helped answer them through meetings, publications, debates and research networks.

Its journals allowed scientists to publish findings, challenge methods and build on one another’s work. The Society’s publications eventually included the Quarterly Journal of the Royal Meteorological Society, which became one of the discipline’s leading scientific journals. Meteorology was no longer simply a hobby for people with rain gauges. It had theories, institutions, professional standards and arguments conducted in footnotes.

The Society also helped connect different branches of British meteorology. In 1921, it amalgamated with the Scottish Meteorological Society, founded in 1856. Scottish observers had played an important role in studying rainfall, storms and regional climate. The merger strengthened a national scientific community while preserving access to valuable networks and records.

Women also contributed to meteorology, although scientific institutions did not always rush to recognise them. One important figure was Eleanor Anne Ormerod, known primarily for her work in economic entomology, who became the Society’s first female fellow in 1878. Her election challenged the assumption that organised science should remain an exclusively male weather system.

During the twentieth century, meteorology changed beyond recognition. Aircraft, radiosondes, radar, satellites and computers allowed scientists to observe the atmosphere in three dimensions and calculate how it might behave. Forecasting moved from hand-drawn charts towards mathematical models capable of processing millions, and later billions, of observations.

Still, technology did not make the Society irrelevant. Quite the opposite happened. As meteorology became more specialised, scientists needed stronger professional networks, respected journals and recognised qualifications. The Society supported conferences, research communication, education and professional accreditation.

Today, it describes itself as an independent authority on weather and climate and remains the United Kingdom’s professional and learned society for meteorology. It awards professional qualifications, including Chartered Meteorologist status, supports researchers and practitioners, and helps people build careers in weather and climate science.

Its mission has also widened. Nineteenth-century members wanted to uncover the laws of climate. Their successors now face a world in which climate change affects agriculture, insurance, public health, energy, transport and national security. Understanding the atmosphere no longer sits politely inside a scientific journal. It shapes political arguments, investment decisions and daily life.

Education has therefore become a major part of the Society’s work. Through programmes such as MetLink, it provides classroom resources, teacher support and climate education materials. It also promotes climate literacy, helping young people distinguish between weather and climate, evidence and opinion, and scientific uncertainty and convenient nonsense.

That distinction matters. A cold Tuesday does not disprove global warming, just as one hot afternoon does not explain the climate system. Weather describes short-term atmospheric conditions. Climate describes patterns measured across longer periods. The two interact, but they are not interchangeable, however confidently someone at a barbecue insists otherwise.

The Society also occupies an interesting position between experts and enthusiasts. Membership is not limited to people who can calculate atmospheric dynamics before breakfast. Amateur observers, students, broadcasters, teachers and anyone with a serious interest in weather can participate. That openness reflects meteorology’s unusual cultural position. It is both a complex science and a subject encountered whenever someone opens the curtains.

Britain did not learn to control the weather. No institution has managed that, despite occasional claims involving cloud seeding, secret machines and suspicious aircraft trails. What Britain learned was how to observe weather collectively, compare evidence and turn atmospheric chaos into increasingly reliable knowledge.

Forecasts still fail occasionally because the atmosphere remains a complicated, unstable system rather than a railway timetable. Yet modern meteorology can warn communities about storms, guide aircraft, protect shipping, manage energy supplies and help farmers plan their work. It can also model future climate risks that earlier observers could scarcely have imagined.

The Royal Meteorological Society helped make this possible by giving weather science a community, a public voice and professional legitimacy. It turned isolated measurements into shared knowledge and a Victorian curiosity into a recognised discipline.