| Thirdly, what are the possible consequences caused by excessive greenhouse effect? It directly results in quick increase of the average global temperature. Today, the increase in the Earth's temperature is increasing with unprecedented speed. To understand just how quickly global warming is accelerating, consider this: during the entire 20th century, the average global temperature increased by about 0.6 degrees Celsius, while by using computer climate models, scientists estimate that by the year 2100 the average global temperature will increase by 1.4 degrees to 5.8 degrees Celsius, which is rather a big leap from the last century. Meanwhile, a majority of the scientists agree that even a small increase in the global temperature would lead to significant climate and weather changes, affecting cloud cover, precipitation, wind patterns, the frequency and severity of storms, and the duration of seasons. | |
| 第三,过量的温室效应可能产生什么样的后果?它直接导致全球气温快速升高。今天,地球的温度以前所未有的速度升高。为了了解全球变暖是如何加速的,大家想想看:全球的平均温度在整个20世纪上升了0.6摄氏度。然而，科学家通过使用计算机气候模式估计到2100年全球平均气温将上升1.4度至5.8摄氏度,这将是从上世纪起发生的相当大的飞跃。与此同时,大多数科学家一致认为, 如果全球温度升高了，即使是一点点，也会导致显著的气候变化和天气变化,影响云量、降水量、风场类型、风暴的发生频率和造成影响的严重程度、以及四季持续的时间。 |
| Thirdly, what are the possible consequences caused by excessive greenhouse effect? It directly results in quick increase of the average global temperature. Today, the increase in the Earth' s temperature is increasing with unprecedented speed. To understand just how quickly global warming is accelerating, consider this: during the entire 20th century, the average global temperature increased by about 0. 6 degrees Celsius, while by using computer climate models, scientists estimate that by the year 2100 the average global temperature will increase by 1. 4 degrees to 5. 8 degrees Celsius, which is rather a big leap from the last century. Meanwhile, a majority of the scientists agree that even a small increase in the global temperature would lead to significant climate and weather changes, affecting cloud cover, precipitation, wind patterns, the frequency and severity of storms, and the duration of seasons. | |
| di san, guo liang de wen shi xiao ying ke neng chan sheng shen me yang de hou guo? ta zhi jie dao zhi quan qiu qi wen kuai su sheng gao. jin tian, di qiu de wen du yi qian suo wei you de su du sheng gao. wei liao liao jie quan qiu bian nuan shi ru he jia su de, da jia xiang xiang kan: quan qiu de ping jun wen du zai zheng ge 20 shi ji shang sheng le 0. 6 she shi du. ran er, ke xue jia tong guo shi yong ji suan ji qi hou mo shi gu ji dao 2100 nian quan qiu ping jun qi wen jiang shang sheng 1. 4 du zhi 5. 8 she shi du, zhe jiang shi cong shang shi ji qi fa sheng de xiang dang da de fei yue. yu ci tong shi, da duo shu ke xue jia yi zhi ren wei, ru guo quan qiu wen du sheng gao le, ji shi shi yi dian dian, ye hui dao zhi xian zhu de qi hou bian hua he tian qi bian hua, ying xiang yun liang jiang shui liang feng chang lei xing feng bao de fa sheng pin lv he zao cheng ying xiang de yan zhong cheng du yi ji si ji chi xu de shi jian. |
| Thirdly, what are the possible consequences caused by excessive greenhouse effect? It directly results in quick increase of the average global temperature. Today, the increase in the Earth' s temperature is increasing with unprecedented speed. To understand just how quickly global warming is accelerating, consider this: during the entire 20th century, the average global temperature increased by about 0. 6 degrees Celsius, while by using computer climate models, scientists estimate that by the year 2100 the average global temperature will increase by 1. 4 degrees to 5. 8 degrees Celsius, which is rather a big leap from the last century. Meanwhile, a majority of the scientists agree that even a small increase in the global temperature would lead to significant climate and weather changes, affecting cloud cover, precipitation, wind patterns, the frequency and severity of storms, and the duration of seasons. | |
| dì sān, guò liàng de wēn shì xiào yìng kě néng chǎn shēng shén me yàng de hòu guǒ? tā zhí jiē dǎo zhì quán qiú qì wēn kuài sù shēng gāo. jīn tiān, dì qiú de wēn dù yǐ qián suǒ wèi yǒu de sù dù shēng gāo. wèi liǎo liǎo jiě quán qiú biàn nuǎn shì rú hé jiā sù de, dà jiā xiǎng xiǎng kàn: quán qiú de píng jūn wēn dù zài zhěng gè 20 shì jì shàng shēng le 0. 6 shè shì dù. rán ér, kē xué jiā tōng guò shǐ yòng jì suàn jī qì hòu mó shì gū jì dào 2100 nián quán qiú píng jūn qì wēn jiāng shàng shēng 1. 4 dù zhì 5. 8 shè shì dù, zhè jiāng shì cóng shàng shì jì qǐ fā shēng de xiāng dāng dà de fēi yuè. yú cǐ tóng shí, dà duō shù kē xué jiā yī zhì rèn wéi, rú guǒ quán qiú wēn dù shēng gāo le, jí shǐ shì yì diǎn diǎn, yě huì dǎo zhì xiǎn zhù de qì hòu biàn huà hé tiān qì biàn huà, yǐng xiǎng yún liàng jiàng shuǐ liàng fēng chǎng lèi xíng fēng bào de fā shēng pín lǜ hé zào chéng yǐng xiǎng de yán zhòng chéng dù yǐ jí sì jì chí xù de shí jiān. |
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