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IELTS Academic Reading Practice Test 99

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 Balloons That Measure the Sky

Modern weather forecasting depends on accurate measurements of the atmosphere far above the ground. Observations made at the surface alone cannot show how temperature, moisture and wind vary with height, yet this information is essential for the computer models that predict the weather and warn of storms. For more than a century, the main instrument for gathering such measurements has been the weather balloon, a relatively inexpensive and robust device that rises through the lower atmosphere carrying small instruments into regions that no aircraft can routinely reach at such low cost.

The deliberate use of balloons to study the atmosphere began in the late nineteenth century. Early attempts employed kites and manned gas balloons, but kites required steady wind and could become tangled on trees, and human aeronauts could not safely remain at great altitudes for long. Meteorologists therefore sought ways to send instruments aloft without carrying people. In the 1890s, weather services in several countries began releasing unmanned balloons fitted with thermometers and barometers, but the readings could only be examined after the balloon had returned to the ground, often many hours or even days later. Despite these early difficulties, interest in upper-air observation grew steadily.

A major advance came in 1902, when the French meteorologist Léon Teisserenc de Bort used repeated instrumented flights to show that air temperature stopped decreasing at a certain point high in the atmosphere. That boundary was later named the tropopause, and the stable layer above it became known as the stratosphere. Balloon soundings had thus revealed the basic vertical structure of the atmosphere for the first time. The discovery encouraged further investment in upper-air observation, although the method still depended on finding fallen instruments, which was extremely difficult in remote or forested country.

The next step was to make the instruments report their readings while the flight was still in progress. During the 1930s, the addition of small radio transmitters to balloon payloads created the radiosonde, a compact package that could send pressure, temperature and humidity data back to a ground station while the balloon continued to climb. This removed the need to recover the instruments and allowed upper-air data to be collected on a regular schedule. Radiosondes were soon produced in large numbers, and national networks began making daily ascents in many parts of the world.

A modern radiosonde is usually lifted by a balloon made from natural latex or synthetic rubber and filled with hydrogen or helium. As the balloon rises, the pressure around it falls steadily, and the balloon expands from about two metres across at launch to the size of a small bus before bursting at an altitude of roughly 30 kilometres. The radiosonde is suspended some distance below the balloon to reduce any influence that the balloon itself might have on the air being sampled. Throughout the ascent, sensors record temperature, humidity and pressure, and many instruments also use satellite navigation signals to calculate wind speed and direction at every level.

Measurements of this kind are made at approximately 900 sites around the world, normally twice a day, at midnight and noon Coordinated Universal Time. Because the balloons are released at the same hours everywhere, the observations form a synchronised global picture of the atmosphere. This global snapshot is essential for the numerical models that produce forecasts ranging from a few hours to more than a week ahead. Under the coordination of the World Meteorological Organization, the data are shared internationally, so that even small countries contribute to and benefit from the observing system.

After a balloon bursts, a small parachute lowers the radiosonde back to the ground. Many radiosondes carry a printed notice asking anyone who finds them to return the instrument to the meteorological service, and a proportion are recovered, checked and prepared for reuse. The vast majority, however, are never found, and the balloons themselves are not reusable. Latex balloons are designed to break down relatively quickly after falling, but in remote areas they can still become visible litter, which has led some operators to look for alternative materials.

Despite its long history, the weather balloon is not a perfect observing tool. A balloon drifts with the wind, so its measurements are not made exactly above the launch site, and the ascent through the atmospheric column can take an hour or more. Balloons also cannot sample the very highest levels of the atmosphere, and each flight gives information along only a narrow path. Satellites provide a much broader view of temperature and moisture over the oceans and other unobserved regions, yet balloon soundings remain valuable because they offer high vertical resolution and because satellite instruments are checked against them.

Some researchers have proposed drones and other aircraft as a potential replacement for weather balloons, and satellites continue to improve. However, no alternative yet matches the balloon's combination of low cost, simplicity and reliability. Their relative cheapness also means that failures are far less damaging than the loss of a specialised aircraft. Gaps in the radiosonde network can noticeably reduce the accuracy of forecasts in the regions affected. For as long as precise upper-air data matter, balloons are likely to remain part of the observing system, carrying out the unglamorous but essential work of telling us what the sky is doing above where we live.

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 table below. Choose ONE WORD AND/OR A NUMBER from the passage for each answer.

Write ONE WORD ONLY for each answer.

The development of upper-air observation

DateDevelopmentConsequence or feature

1890s

Unmanned balloons

Readings could only be examined after the had returned to the ground

1902

Teisserenc de Bort's flights

Revealed the atmosphere's basic vertical

1930s

Radiosonde

Sent pressure, temperature and humidity back to a ground station

Present

Modern balloons

Expand to the size of a small before bursting

Present

Balloon network

Ascents made twice a day at about sites

After flight

Parachute

Some radiosondes are recovered and prepared for

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.

Kites used for upper-air observation needed a steady wind.
Early balloon studies of the atmosphere always carried a human observer.
Teisserenc de Bort used a single balloon flight to discover the tropopause.
Modern balloons are filled with a mixture of hydrogen and helium.
Radiosondes are attached directly to the balloon to ensure accurate readings.
Weather balloon observations are shared between countries through an international organisation.
The vast majority of radiosondes are returned to meteorological services.

About this reading test

A full IELTS Academic Reading practice test with 40 questions on three original passages: how weather balloons collect upper-air data, the human capacity for endurance running, and what research really shows about decision fatigue. Includes a timer, band estimate and explanations.

PartPassageQuestionsQuestion typesTopicsWords
1The Balloons That Measure the Sky1–13Table completion, True / False / Not GivenEarth & Geography, Science879
2The Running Ape14–26Matching information, Multiple choice (choose more than one), Summary completionScience, Sport & Leisure901
3The Price of Choosing27–40Multiple choice, Yes / No / Not Given, Sentence completionPsychology, Science920

How to use this practice test

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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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