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Thunder Board: low-cost 8-bit ISA Sound Blaster compatible sound. Thunder and Lightning: VGA adapter with Sound Blaster compatible sound. PCMCIA 16 Bit Sound Card; Pro Audio Studio 16: enhanced version of the Pro Audio Spectrum 16 sound card, bundled with voice-recognition software and a microphone
Thunder is the sound caused by lightning. [1] [2] [3] Depending upon the distance from and nature of the lightning, it can range from a long, low rumble to a sudden, loud crack. The sudden increase in temperature and hence pressure caused by the lightning produces rapid expansion of the air in the path of a lightning bolt. [4]
Castle thunder is a sound effect that consists of the sound of a loud thunderclap during a rainstorm. It was originally recorded for the 1931 film Frankenstein , and has since been used in dozens of films, television programs, and commercials.
The heavy snowfall tends to muffle the sound of the thunder so that it sounds more like a low rumble than the loud, sharp bang that is heard during regular thunderstorms. [2] Thundersnow can occur during a normal snowstorm that sustains strong vertical mixing which allows for favorable conditions for lightning and thunder to occur.
A young boy named Sam prepares to go to sleep with his bedroom light off for the first time, but quickly becomes frightened by the darkness. Inspired by the bravery of his superhero idol, Pajama Man, Sam assumes the role of Pajama Sam by donning a red cape, purple mask, and gathering equipment to confront the darkness, which he believes to be an actual living being.
Direct strike: lightning directly hits the person Orifice entry: may occur if lightning strike occurs near the head entering eyes, ears and mouth to flow internally; Side splash: lightning jumps from the location of primary strike to a nearby person; Contact injury: injury that occurs when a person is touching an object on the pathway of lightning
Lightning is a natural phenomenon, more specifically an atmospheric electrical phenomenon. It consists of electrostatic discharges occurring through the atmosphere between two electrically charged regions, either both existing within the atmosphere or one within the atmosphere and one on the ground, with these regions then becoming partially or wholly electrically neutralized.
VLF spectrogram of an electromagnetic whistler wave, as received by the Stanford University VLF group's wave receiver at Palmer Station, Antarctica.. A whistler is a very low frequency (VLF) electromagnetic (radio) wave generated by lightning. [1]
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