Pregunta 1
Transcripción del audio (en la app lo escuchas con voz)
Narrator: Part 4. You will hear part of a lecture on urban heat islands.
Lecturer: Good afternoon. Today I'm going to talk about a phenomenon that affects almost every large city in the world: the urban heat island. The term was first used several decades ago, but the effect itself had been noticed long before that, when early weather observers found that their city thermometers consistently gave higher readings than those placed in nearby farms and villages. In short, the urban heat island describes the way in which a city is noticeably warmer than the surrounding countryside. The difference can be several degrees. Now, you might expect the gap to be widest in the afternoon, when the sun is at its strongest. In fact, the opposite is true. During the day, both the city and the rural areas heat up. It's at night that the difference really shows, because the countryside cools quickly while the city slowly releases the heat it has stored.
Lecturer: So what causes it? Researchers generally identify four main factors, and I'll take them in turn. The first is the materials we build with. Brick, concrete and stone all hold heat, but the worst offender is the dark surface that covers most of our roads and many flat roofs – I mean asphalt. It absorbs a great deal of the sun's energy during the day and, rather like a storage heater, keeps it for hours afterwards.
Lecturer: The second factor is the lack of vegetation. In rural areas, a great deal of the sun's energy is used not to heat the ground but to turn water into vapour. As water evaporates from leaves and from damp soil, it draws heat out of the surrounding air. Evaporation, in other words, works as a kind of natural air conditioner. In a city covered in concrete, rainwater runs straight into the drains, there's very little moisture left at the surface, and so that natural cooling is largely lost.
Lecturer: Third, there's the shape of the city itself. Planners sometimes talk about 'urban canyons' – narrow streets lined by tall buildings. These are very good at trapping heat. The sun's energy bounces from one wall to another instead of escaping to the sky, and, just as importantly, tall buildings standing close together block the wind, so the warm air simply sits there instead of being carried away.
Lecturer: And finally, cities produce a lot of heat of their own. In the past the main sources were vehicles and factories, and they still contribute. But increasingly, a large share comes from air conditioning, which, ironically, cools the inside of buildings by pumping heat out into the streets – making the outdoor problem worse and, of course, increasing the demand for more air conditioning.
Lecturer: Why does all this matter? Well, higher temperatures increase the demand for energy, and they also speed up the chemical reactions that create certain air pollutants, such as ground-level ozone. But the most serious effect is on health. During heatwaves, the risk of illness rises sharply. Young children are often mentioned in this context, and they do need protection, but the research shows that the group at greatest risk is elderly people, who are less able to regulate their body temperature and who often live alone.
Lecturer: Fortunately, there's a good deal that cities can do. One of the simplest measures is the so-called cool roof. Instead of absorbing the sun's energy, a roof painted in a light colour can reflect much of it back into the sky. The cost is low, and studies have found that the temperature inside the top floor of a building can fall noticeably as a result.
Lecturer: Trees are another powerful tool. Most people think of them simply in terms of shade, and shade is certainly valuable. But trees also cool the air directly, by releasing moisture through their leaves – the same process I described earlier. Parks, green roofs and even small street gardens can all help in the same way, though a single large tree generally does more than a lawn of the same area.
Lecturer: However, a city can't do everything at once, so it needs to decide where to act first. For that, planners need detailed maps of temperature across the whole city. Ground-level measurements are expensive to collect, so these are now usually produced using data from satellites. And what they reveal is often uncomfortable: the hottest neighbourhoods tend to be the poorest ones, with the fewest trees and the most closely packed housing. In the second half of today's session, we'll look at how two cities have used this information to decide their priorities.
Questions 38–40. Complete the sentences below. Write ONE WORD ONLY for each answer.
38. Instead of absorbing solar energy, light-coloured roofs (38) ______ a large part of it.
39. Apart from providing shade, trees lower the air temperature by giving off (39) ______ through their leaves.
40. Before deciding where to act first, planners need detailed temperature (40) ______ of the whole city.
Ver respuesta y explicación
- (38) reflect
- (39) moisture
- (40) maps
Explicación
38: 'a roof painted in a light colour can reflect much of it back into the sky' – 'absorb' is the opposite. 39: trees 'cool the air directly, by releasing moisture through their leaves'; shade is the point most people think of. 40: 'planners need detailed maps of temperature across the whole city'; satellites are the source of the data, not what planners need.