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IELTS Academic Reading Practice Test 77

Part 1 · Read the text and answer questions 1–13

You should spend about 20 minutes on Questions 1–13, which are based on Reading Passage 1 below.

The Science of Weather Prediction

Modern weather forecasting is often taken for granted, but its reliability rests on a quiet scientific revolution. This change took more than a century and is still not complete. Every day, forecasts guide choices about transport, farming, energy and safety. Yet because the atmosphere is a chaotic fluid, prediction is never straightforward. A forecast is a statement of chance based on huge amounts of data and on mathematical models of the atmosphere, ocean and land. This is why weather services now operate around the clock.

For most of history, people read the clouds, winds and changing pressure with only the naked eye. The thermometer, barometer and hygrometer made readings better, but information moved no faster than a horse. These tools recorded readings in a steady way, but they did not solve the speed problem. In the nineteenth century the electric telegraph made it possible to gather weather observations from many places at once, and in the 1860s the British naval officer Robert FitzRoy used coastal telegraph reports to issue the first public weather forecasts. His warnings were sometimes ridiculed, yet they showed that early notice could save lives. FitzRoy also set up the first storm warning service for ships, a step that later became routine.

Modern scientific forecasting began with the equations of physics. Around 1900, Vilhelm Bjerknes, a Norwegian meteorologist, formulated a set of equations that govern the behaviour of the atmosphere. Bjerknes argued that forecasting was a problem in mathematical physics, but the computational demands were enormous. In 1922 the British scientist Lewis Fry Richardson tried to calculate a weather forecast by hand from such equations. The work took him weeks and produced a wildly unrealistic result, largely because errors in the initial data distorted the calculations. Richardson still imagined a 'forecast factory' in which thousands of human computers would keep pace with the weather.

After the Second World War, digital computers changed the situation. The stored-program computer made automatic calculation possible for the first time. In 1950 a team led by Jule Charney used the ENIAC computer to integrate the atmospheric equations forward in time step by step. The result was the first successful numerical weather prediction. It showed that Richardson's method was sound, but that only a machine could carry out the enormous number of calculations required. The calculation was later done again at higher detail as machines improved.

The next advance came from an unexpected source. In the 1960s, Edward Lorenz was experimenting with a simple computer model when he discovered that tiny differences in starting values could produce completely different weather patterns. This sensitivity, often called the butterfly effect, means that small errors in observations grow rapidly. It sets a basic limit on how far ahead useful forecasts can reach. Even with perfect data, the limit would remain, but better data can extend the useful range.

Modern forecasters rely on a large global observing network. Surface stations, ships, buoys and aircraft report temperature, pressure, humidity and wind. Balloon-borne radiosondes sample the upper air, while satellites and radar provide continuous coverage of clouds, rain and storms. Radiosondes are sent up twice a day from sites around the world, giving vertical profiles of the air. The first weather satellite, TIROS-1, was launched in 1960, and satellite data have been part of routine forecasting ever since. Today, geostationary and polar-orbiting satellites watch the globe around the clock.

All these observations must be joined with a model. Data assimilation blends the latest observations with a short-range model forecast to produce the best guess of the current state of the air. The model then splits the air into a grid of millions of boxes and solves the motion equations for each box. Supercomputers do trillions of operations a second to move the weather forward in time. The grid spacing of such models has fallen from hundreds of kilometres in the 1960s to just a few kilometres today.

Because the air is chaotic, a single forecast is not reliable far ahead. Ensemble forecasting deals with this by running the model many times, each with slightly different starting conditions or with slightly different model settings. If most members agree a storm will form, forecasters can warn with high confidence. If the members disagree, the outlook remains uncertain. The spread among members shows how unsure the forecast is.

This mix of better data, faster computers and ensemble methods has brought steady gains. A five-day forecast from a modern centre is now about as accurate as a three-day forecast was a generation ago. Skill in predicting tropical storm tracks has increased, while forecasts of storm intensity have improved more slowly. Nevertheless, certain phenomena remain difficult. Local thunderstorms, fog and the rapid deepening of tropical cyclones can still surprise even the most advanced systems. Because such features are small and short-lived, they push the limits of both observation and model detail.

Research is now turning to machine learning, which may speed up some calculations and improve the use of past data. Some new systems have shown skill comparable to conventional models for short-range prediction, but they are still being tested in operational use. Yet no algorithm can remove the butterfly effect. The air will always contain uncertainty, and forecasts will therefore always be, in essence, statements of chance. Human judgement remains important, especially when automated guidance is unclear or conflicting.

Tip: select any text in the passage to highlight it in one of four colours. Click a highlight to remove it.

Questions 1–6◎ Practise this set only

Complete the notes below. Choose ONE WORD ONLY from the passage for each answer.

Write ONE WORD ONLY for each answer.

The road to numerical weather prediction

Early public forecasts by Robert FitzRoy used observations sent by . Vilhelm Bjerknes later formulated the that describe the atmosphere. Lewis Fry Richardson attempted to produce a forecast by from such equations, but the result was unrealistic. In 1950 Charney's team used ENIAC to move the equations forward in step by step. Modern data assimilation blends fresh with a short-range model prediction. Ensemble forecasting tests the effect of using slightly different starting .

Questions 7–13◎ Practise this set only

Do the following statements agree with the information given in Reading Passage 1? Choose TRUE if the statement agrees with the information, FALSE if the statement contradicts the information, or NOT GIVEN if there is no information on this.

Before the invention of the electric telegraph, weather information could not travel faster than a horse.
FitzRoy was dismissed from his post because his forecasts were inaccurate.
Richardson's forecast failed because his equations were physically incorrect.
Lorenz made his discovery while working with a basic computer simulation.
The butterfly effect means that forecasts become more accurate as time passes.
Weather satellites have been used regularly by forecasters since 1960.
Modern forecasts can predict exactly where and when a local thunderstorm will occur several days in advance.

About this reading test

A full IELTS Academic Reading practice test with 40 questions on three original passages: the science of weather forecasting, the promise and risks of de-extinction, and the case for public funding of the arts. Includes a timer, band estimate and explanations.

PartPassageQuestionsQuestion typesTopicsWords
1The Science of Weather Prediction1–13Note completion, True / False / Not GivenEarth & Geography, Science886
2The Promise and Peril of De-extinction14–26Matching information, Multiple choice (choose more than one), Summary completionScience, Environment, Animals902
3The Case for Public Support of the Arts27–40Multiple choice, Yes / No / Not Given, Summary completion (word list)Arts & Culture, Business & Economics, Society937

How to use this practice test

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  • For gap-fill questions, keep to the word limit; an answer over the limit is marked wrong, as in the real exam.

All passages and questions on Sprechify are written by our own team in the official IELTS format. They are not taken from Cambridge IELTS books or any other published test. Band scores are estimates based on the conversion commonly used for practice tests.

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