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學(xué)生介紹天氣的高中英語(yǔ)作文
介紹天氣的作文不好寫(xiě)，特別還是英語(yǔ)作文。下面就是百分網(wǎng)小編給大家整理的.學(xué)生介紹天氣的英語(yǔ)作文，希望大家喜歡。
學(xué)生介紹天氣的英語(yǔ)作文(一)
The weather is a set of all the phenomena in a given atmosphere at a given time. It also includes interactions with the hydrosphere. The term usually refers to the activity of these phenomena over short periods (hours or days), as opposed to the term climate, which refers to the average atmospheric conditions over longer periods of time. When used without qualification, "weather" is understood to be the weather of Earth.
Weather most often results from temperature differences from one place to another. On large scales, temperature differences occur because areas closer to the equator receive more energy per unit area from the Sun than do regions closer to the poles. On local scales, temperature differences can occur because different surf-aces (such as oceans, forests, ice sheets, or man-made objects) have differing physical characteristics such as reflectivity, roughness, or moisture content.
Surf-ace temperature differences in turn cause pressure differences. A hot surf-ace heats the air above it and the air expands, lowering the air pressure. The resulting horizontal pressure gradient accelerates the air from high to low pressure, creating wind, and Earth's rotation then causes curvature of the flow via the Coriolis effect. The si-mp-le systems thus formed can then display emergent behaviour to produce more complex systems and thus other weather phenomena. Large scale examples include the Hadley cell while a smaller scale example would be coastal breezes.
The strong temperature contrast between polar and tropical air gives rise to the jet stream. Most weather systems in the mid-latitudes are caused by instabilities of the jet stream flow (see baroclinity). Weather systems in the tropics are caused by different processes, such as monsoons or organized thunderstorm systems.
Because the Earth's axis is tilted relative to its orbital plane, sunlight is incident at different angles at different times of the year. In June the Northern Hemisphere is tilted towards the sun, so at any given Northern Hemisphere latitude sunlight falls more directly on that spot than in December (see Effect of sun angle on climate). This effect causes seasons. Over thousands to hundreds of thousands of years, changes in Earth's orbital parameters affect the amount and distribution of solar energy received by the Earth and influence long-term climate (see Milankovitch cycles).
On Earth, common weather phenomena include such things as wind, cloud, rain, snow, fog and dust storms. Lecommon events include natural disasters such as tornadoes, hurricanes and ice storms. Almost all familiar weather phenomena occur in the troposphere (the lower part of the atmosphere). Weather does occur in the stratosphere and can affect weather lower down in the troposphere, but the exact mechanisms are poorly understood.[1]
The atmosphere is a chaotic system, so small changes to one part of the system can grow to have large effects on the system as a whole. This makes it difficult to accurately predict weather more than a few days in advance, though weather forecasters are continually working to extend this limit through the scientific study of weather, meteorology. It is theoretically impossible to make useful day-to-day predictions more than about two weeks ahead, imposing an upper limit to potential for improved prediction skill.[1] Chaos theory says that the slightest variation in the motion of the ground can grow with time. This idea is sometimes called the butterfly effect, from the idea that the motions caused by the flapping wings of a butterfly eventually could produce marked changes in the state of the atmosphere. Because of this sensitivity to small changes it will never be possible to make perfect forecasts, although there still is much potential for improvement.
The sun and oceans can also affect the weather of land. If the sun heats up ocean waters for a period of time, water can evaporate. Once evaporated into the air, the moisture can spread throughout nearby land, thus ma-ki-ng it cooler.
學(xué)生介紹天氣的英語(yǔ)作文(二)
Good evening ! Here’s the next day weather report for some main cities in Guangxi. Nanning is sunny. It is hot with the temperature from 20℃ to29℃. In Guilin, its temperature is arranged from 8℃to 13℃. It’s cold in the morning and at night. peole should wear more clothes in case of catching cold. Liuzhou is cloudy in the daytime and has a strong wind during the night time with the temperature from 11℃to 15℃. There will be beautiful sunshine in Wuzhou. People will feel comfortable to go out as the temperature is from 15℃to 22℃.That’s the weather report for today . Thank you for listening .
晚上好!這是廣西的一些主要城市第二天的天氣預(yù)報(bào)。南寧是晴天，很熱。氣溫是20℃到29℃。桂林的溫度是8℃到13℃。早上和晚上比較冷。以防感冒人們應(yīng)該多穿點(diǎn)衣服。柳州白天多云，晚上有強(qiáng)風(fēng)，溫度是11℃到15℃。梧州陽(yáng)光燦爛。溫度是15℃到22℃。人們外出會(huì)感覺(jué)到很舒適。這是今天的天氣報(bào)告。謝謝您的傾聽(tīng)。
學(xué)生介紹天氣的英語(yǔ)作文(三)
Let's take a look at the weather in Shanxi Province for the next 24 hours. Taiyuan would be cloudy at the time with the temperature from eighteen to twenty-eight. A strong wind would reach Datong, which could cause much rain, The temperature would be sixteen to twenty-six. Yangquan would be sunny with the highest temperature of thirty degree. Linfen would be windy and its temperature would be twenty-three to thirty-two. We would have a sunny and hot day in Yuncheng. Its temperature would stay between twenty-eight to thirty-four.
Good morning ! Here’s the weather report for some big cities in the world . Beijing is cloudy . It’s very cold, so wear warm clothes when you go out . In Hong Kong there’s beautiful sunshine.(陽(yáng)光燦爛). People will feel cool in the daytime. It is sunny in New York , but there’s a strong wind (大風(fēng)) in the afternoon. It will be rainy in Sydney but very hot. The day after tomorrow (后天) will be sunny.
That’s the weather report for today . Thank you for listening .(謝謝收聽(tīng))
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