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2. What Is Thunder and Lightning?Li

2. What Is Thunder and Lightning?


Lightning is a sudden, violent flash of electricity between a cloud and the ground, or from cloud to cloud. A lightning fl ash, or bolt, can be several miles long. It is so hot, with an average temperature of 34,000° Centigrade, that the air around it suddenly expands with a loud blast. This is the thunder we hear.

Lightning occurs in hot, wet storms. Moist air is driven up to a great height. It forms a type of cloud called cumulonimbus. When the cloud rises high enough, the moisture freezes and ice crystals and snowfl akes are formed. These begin to fall, turning to rain on the way down. This rain meets more moist air rising, and it is the friction between them which produces static electricity. When a cloud is fully charged with this electricity, it discharges it as a lightning flash.


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2. What Is Thunder and Lightning?Lightning is a sudden, violent flash of electricity between a cloud and the ground, or from cloud to cloud. A lightning fl ash, or bolt, can be several miles long. It is so hot, with an average temperature of 34,000° Centigrade, that the air around it suddenly expands with a loud blast. This is the thunder we hear.Lightning occurs in hot, wet storms. Moist air is driven up to a great height. It forms a type of cloud called cumulonimbus. When the cloud rises high enough, the moisture freezes and ice crystals and snowfl akes are formed. These begin to fall, turning to rain on the way down. This rain meets more moist air rising, and it is the friction between them which produces static electricity. When a cloud is fully charged with this electricity, it discharges it as a lightning flash.
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2. Apa Guntur dan petir? Petir adalah tiba-tiba, flash kekerasan listrik antara awan dan tanah, atau dari awan ke awan. Sebuah abu fl petir, atau baut, dapat beberapa mil panjang. Hal ini sangat panas, dengan suhu rata-rata 34.000 ° Celcius, bahwa udara di sekitarnya tiba-tiba mengembang dengan ledakan keras. Ini adalah guntur kita dengar. Petir terjadi di tempat yang panas, badai basah. Udara lembab didorong hingga ketinggian yang besar. Membentuk jenis awan cumulonimbus yang disebut. Ketika awan naik cukup tinggi, membeku kelembaban dan kristal es dan snowfl akes terbentuk. Ini mulai jatuh, beralih ke hujan dalam perjalanan ke bawah. Hujan ini memenuhi lebih lembab udara naik, dan itu adalah gesekan antara mereka yang menghasilkan listrik statis. Ketika awan terisi penuh dengan listrik ini, maka akan dibuang sebagai kilat.







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