Thunder in Different Languages: Thunder is the sound brought about by lightning. It can range from a sharp, boisterous split to a long, low thunder, depending on the good way and nature of lightning (brontide). The steep increase in lightning weight and temperature causes the air inside to spread quickly and includes the way a flash. This evolution of air therefore makes a sonic stun wave, often referred to as a “thunderclap” or “ring of thunder.”
How to Say Thunder in 88 Different Languages
| Different Languages | Word Thunder |
|---|---|
| Albanian | bubullimë |
| Basque | trumoiak |
| Belarusian | гром |
| Bosnian | grmljavina |
| Bulgarian | гръм |
| Catalan | tro |
| Croatian | grmljavina |
| Czech | hrom |
| Danish | torden |
| Dutch | donder |
| Estonian | kõu |
| Finnish | ukkonen |
| French | tonnerre |
| Galician | trono |
| German | Donner |
| Greek | βροντή (vrontí) |
| Hungarian | mennydörgés |
| Icelandic | Þrumuveður |
| Irish | toirneach |
| Italian | tuono |
| Latvian | pērkons |
| Lithuanian | perkūnas |
| Macedonian | ГРОМ |
| Maltese | Thunder |
| Norwegian | torden |
| Polish | grzmot |
| Portuguese | trovão |
| Romanian | tunet |
| Russian | гром (grom) |
| Serbian | гром (grom) |
| Slovak | hrom |
| Slovenian | grmenje |
| Spanish | trueno |
| Swedish | åska |
| Ukrainian | грім (hrim) |
| Welsh | Thunder |
| Yiddish | דונער |
| Armenian | որոտ |
| Azerbaijani | şimşək |
| Bengali | বজ্রধ্বনি |
| Chinese Simplified | 雷 (léi) |
| Chinese Traditional | 雷 (léi) |
| Georgian | ქუხილი |
| Gujarati | ગર્જના |
| Hindi | बिजली |
| Hmong | xob quaj |
| Japanese | サンダー |
| Kannada | ಗುಡುಗು |
| Kazakh | күркіреу |
| Khmer | ផ្គរលាន់ |
| Korean | 우뢰 (uloe) |
| Lao | thunder |
| Malayalam | ഇടി |
| Marathi | मेघगर्जना |
| Mongolian | аянга |
| Myanmar (Burmese) | မျိုးချုန်းသံ |
| Nepali | गर्जन |
| Sinhala | ගිගුරුම් සහිත |
| Tajik | тундар |
| Tamil | இடி |
| Telugu | ఉరుములు |
| Thai | ฟ้าร้อง |
| Turkish | gök gürültüsü |
| Urdu | گرج |
| Uzbek | momaqaldiroq |
| Vietnamese | sấm sét |
| Arabic | صوت الرعد (sawt alraed) |
| Hebrew | רַעַם |
| Persian | رعد |
| Afrikaans | donderweer |
| Chichewa | bingu |
| Hausa | aradu |
| Igbo | égbè eluigwe |
| Sesotho | sealuma |
| Somali | onkod |
| Swahili | radi |
| Yoruba | ãra |
| Zulu | nokuduma |
| Cebuano | dalugdog |
| Filipino | kulog |
| Indonesian | guntur |
| Javanese | gludhug |
| Malagasy | kotrokorana |
| Malay | guruh |
| Maori | whatitiri |
| Esperanto | tondro |
| Haitian Creole | loraj |
| Latin | tonitrua, |
This evolution of air thus causes a sound stun wave, which is often referred to as a thunderclap. Hundreds of years of theoretical and logical research has been the reason for the thunder. It was early thought by Gods, but old Greek logicians attributed that to frequent causes, e.g. the striking wind disputes and air development inside struggles.
The roman thinker Lucretius said it was inside the clouds from the sound of hail. The recognized assumption in the mid-nineteenth century was that the light created a vacuum; that the disintegration of this vacuum produced the so-called thunder. In the twentieth century an accord advanced that thunder must start with a stun wave noticeable all around because of the unexpected warm development of the plasma in the lightning channel.
The temperature inside the lightning channel, estimated by unearthly examination, fluctuates during its 50 μs presence, rising strongly from an underlying temperature of around 20,000 K to around 30,000 K, at that point dropping ceaselessly step by step to around 10,000 K. The normal is around 20,400 K (20,100 °C; 36,300 °F).
This warming results in a rapid external evolution that affects the cooler air, at a velocity faster than any other movement would be. The resultant outward-moving heartbeat is a stun wave, comparable on a basic level to the stun wave-shaped by a blast, or at the front of a supersonic airplane. Trial studies of recreated lightning have produced very consistent results with this model, but the exact physical systems of the procedure proceed with flattery.
Other causes have additionally been proposed, depending on electrodynamic impacts of the huge current following up on the plasma in the electrical jolt The most recognizable part of lightning and thunder is that the lightning is seen before the thunder is heard. The result is that light has a much more remarkable speed than sound speed.
Sound in dry air is around 343 m/s or 1,127 ft/s or 768 mph (1,236 km/h) at 20 °C (68 °F). An extremely splendid glimmer of lightning and a practically synchronous sharp “break” of thunder, a thundercrack, in this manner demonstrates that the lightning strike was exceptionally close.
