| Warm water and moist , warm air are two main factors that are responsible for causing hurricane storms. Hurricanes occur when the moist, warm air from the surface of the ocean rises and meets the cooler air. There is also release of hidden heat due to cooling process, which increases the temperature of the cooler air above. In the cycle, more warm, humid air rises and joins the developing storm. Hence, there is a transfer of heat from the surface of the ocean to the atmosphere above. As the cycle of exchanging heat continues, a wind pattern is created that moves in a twisting fashion around a calm center, which is called as the hurricane eye. The increased circulation of warm, humid air enhances the speed of wind. Another factor that increases the speed of wind is high-pressure air at high altitude. As this high-pressure air moves to the center and meets the low-pressure air, the wind speed again increases. | |
| 温暖的海水和暖湿气流是飓风形成的两大要素，当海洋表面的暖湿气流与冷空气交汇就会形成飓风。也有可能是冷却系统使隐藏的热量释放出来导致的。在飓风形成的圈中，更多的暖湿空气被聚集加入到不断成长的飓风中。因此，有一种海洋表面的热量到海洋上空气候的转换。在不断转换热量的循环中，创造了一种风围绕着冷中心——台风眼旋转移动的模式。被加剧循环的冷湿空气提高了风的移动速度。另一个提高风速的因素来自高海拔的空气高压。当高压空气移动到中心并与低压空气相交汇，风速再次被提高。 |
| Warm water and moist , warm air are two main factors that are responsible for causing hurricane storms. Hurricanes occur when the moist, warm air from the surface of the ocean rises and meets the cooler air. There is also release of hidden heat due to cooling process, which increases the temperature of the cooler air above. In the cycle, more warm, humid air rises and joins the developing storm. Hence, there is a transfer of heat from the surface of the ocean to the atmosphere above. As the cycle of exchanging heat continues, a wind pattern is created that moves in a twisting fashion around a calm center, which is called as the hurricane eye. The increased circulation of warm, humid air enhances the speed of wind. Another factor that increases the speed of wind is highpressure air at high altitude. As this highpressure air moves to the center and meets the lowpressure air, the wind speed again increases. | |
| wen nuan de hai shui he nuan shi qi liu shi ju feng xing cheng de liang da yao su, dang hai yang biao mian di nuan shi qi liu yu leng kong qi jiao hui jiu hui xing cheng ju feng. ye you ke neng shi leng que xi tong shi yin cang de re liang shi fang chu lai dao zhi de. zai ju feng xing cheng de quan zhong, geng duo de nuan shi kong qi bei ju ji jia ru dao bu duan cheng zhang de ju feng zhong. yin ci, you yi zhong hai yang biao mian di re liang dao hai yang shang kong qi hou de zhuan huan. zai bu duan zhuan huan re liang de xun huan zhong, chuang zao le yi zhong feng wei rao zhe leng zhong xin tai feng yan xuan zhuan yi dong de mo shi. bei jia ju xun huan de leng shi kong qi ti gao le feng de yi dong su du. ling yi ge ti gao feng su de yin su lai zi gao hai ba de kong qi gao ya. dang gao ya kong qi yi dong dao zhong xin bing yu di ya kong qi xiang jiao hui, feng su zai ci bei ti gao. |
| Warm water and moist , warm air are two main factors that are responsible for causing hurricane storms. Hurricanes occur when the moist, warm air from the surface of the ocean rises and meets the cooler air. There is also release of hidden heat due to cooling process, which increases the temperature of the cooler air above. In the cycle, more warm, humid air rises and joins the developing storm. Hence, there is a transfer of heat from the surface of the ocean to the atmosphere above. As the cycle of exchanging heat continues, a wind pattern is created that moves in a twisting fashion around a calm center, which is called as the hurricane eye. The increased circulation of warm, humid air enhances the speed of wind. Another factor that increases the speed of wind is highpressure air at high altitude. As this highpressure air moves to the center and meets the lowpressure air, the wind speed again increases. | |
| wēn nuǎn de hǎi shuǐ hé nuǎn shī qì liú shì jù fēng xíng chéng de liǎng dà yào sù, dāng hǎi yáng biǎo miàn dí nuǎn shī qì liú yǔ lěng kōng qì jiāo huì jiù huì xíng chéng jù fēng. yě yǒu kě néng shì lěng què xì tǒng shǐ yǐn cáng de rè liàng shì fàng chū lái dǎo zhì de. zài jù fēng xíng chéng de quān zhōng, gèng duō de nuǎn shī kōng qì bèi jù jí jiā rù dào bù duàn chéng zhǎng de jù fēng zhōng. yīn cǐ, yǒu yī zhǒng hǎi yáng biǎo miàn dí rè liàng dào hǎi yáng shàng kōng qì hòu de zhuǎn huàn. zài bù duàn zhuǎn huàn rè liàng de xún huán zhōng, chuàng zào le yī zhǒng fēng wéi rào zhe lěng zhōng xīn tái fēng yǎn xuán zhuǎn yí dòng de mó shì. bèi jiā jù xún huán de lěng shī kōng qì tí gāo le fēng de yí dòng sù dù. lìng yí gè tí gāo fēng sù de yīn sù lái zì gāo hǎi bá de kōng qì gāo yā. dāng gāo yā kōng qì yí dòng dào zhōng xīn bìng yǔ dī yā kōng qì xiāng jiāo huì, fēng sù zài cì bèi tí gāo. |
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