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SoundBox HD

56.1MB
SBHD-THMT02: Thunder Mountain II (HD)
$20.00
A mountain thunder feast. Includes impressive thunder claps, mighty rolling rumbles, energetic distant boomers and threatening approaching storms. From The Recordist Thunderstorm HD SFX Library. 10 Files.

Included in the above SoundBox are 16Bit-44.1kHz, 24Bit-48kHz and 24Bit-96kHz Broadcast WAV files embedded with Soundminer 4 metadata. The files are compressed/collected in multiple .zip files for ease of download. File sizes for 48kHz and 96kHz are substantially larger than 44.1kHz.

027.4MB - 16-Bit/44.1k - SB_THMT02_THUNDER_MNT2.zip
056.1MB - 24-Bit/48.0k - SBHD48_THMT02_THUNDER_MNT2.zip
24-Bit / 96kHz Broadcast WAV files available upon request.

SBHD-THMT02: Thunder Mountain II (HD) (PDF)
Time
Thunder: Distant Rolling Thunder Clap, Slight Wind 00:35.503
Thunder: Distant Rolling Thunder Clap, Slight Wind 00:36.362
Thunder: Distant Rolling Thunder With Heavy Rumble 00:26.819
Thunder: Large Thunder Clap With Rumble, Distant Rolling Rumble 00:09.450
Thunder: Large Thunder Crack With Heavy Rumble 00:15.464
Thunder: Large Thunder Crack With Heavy Rumble 00:20.015
Thunder: Thunder: Distant Boom And Rumble 00:27.074
Thunder: Thunder: Distant Boom And Rumble 00:14.048
Thunder: Thunderstorm: Distant Storm Approaching 00:23.916
Thunder: Thunderstorm: Distant Storm Approaching 00:28.723


SB-THFR01: Thunder Fury - From our Thunder HD SFX Library (HD)
Thunder gone mad! Intense and powerful thunder strikes and claps. 24Bit-96kHz.
Details $20.00


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This work is made and sold under license. By accepting this work, you agree to the following terms and conditions. Your use of this work is limited and restricted solely for the purpose of synchronizing recordings there from in timed relation with films, training or marketing presentations, radio and television presentations or commercials, and any other multimedia, audiovisual or computer generated displays, programs or presentations. Neither you nor anyone else may make any copies of any of the recordings on this work, except as may be designated to a single stand alone workstation for the purpose of specific audio and/or visual synchronization at your own facility. Transfer, copying or duplication of the work in whole or in part for any other purpose is expressly prohibited unless specifically authorized in writing by The Recordist. Transfer of one or more sounds to any format allowing network or remote access by two or more endusers requires a MultiUser License. Contact The Recordist for details. In the event of a breach of these terms, action may be taken against you directly by the owner of the copyright.

Thunder is the sound made by lightning. Depending on the nature of the lightning and distance of the listener, it can range from a sharp, loud crack to a long, low rumble (brontide). The sudden increase in pressure and temperature from lightning produces rapid expansion of the air surrounding and within a bolt of lightning. In turn, this expansion of air creates a sonic shock wave which produces the sound of thunder. Fear of thunder is known as ceraunophobia.

Cause
The cause of thunder has been the subject of centuries of speculation and scientific inquiry. The first recorded theory is attributed to the Greek philosopher Aristotle in the third century BC, and an early speculation was that it was caused by the collision of clouds. Subsequently, numerous other theories have been proposed. By the mid-19th century, the accepted theory was that lightning produced a vacuum. In the 20th century a consensus evolved that thunder must begin with a shock wave in the air due to the sudden thermal expansion of the plasma in the lightning channel. In a fraction of a second the air is heated to a temperature approaching 28,000 °C (50,000 °F). This heating causes it to expand outward, plowing into the surrounding cooler air at a speed faster than sound would travel in that cooler air. The outward-moving pulse that results is a shock wave, similar in principle to the shock wave formed by an explosion, or at the front of a supersonic aircraft. More recently, this consensus has been eroded by the observation that measured overpressures in simulated lightning are greater than what could be achieved by the amount of heating found. Alternative proposals rely on electrodynamic effects of the massive current acting on the plasma in the bolt of lightning.

Calculating distance
A flash of lightning, followed after some seconds by a rumble of thunder is, for many people, the first illustration of the fact that sound travels more slowly than light. Using this difference, one can estimate how far away the bolt of lightning is by timing the interval between seeing the flash and hearing thunder. The speed of sound in dry air is approximately 343 m/s or 1,127 feet per second or 768 mph (1,236 km/h) at 68°F (20 °C). The speed of light is high enough that it can be taken as infinite in this calculation. Therefore, the lightning is approximately one kilometer distant for every 2.9 seconds (or one mile for every 4.6 seconds). In the same five seconds the light could have circled the globe 37 times. Thunder is seldom heard at distances over 24 kilometers (15 miles). A flash of lightning and a simultaneous sharp "clap!" of thunder, a thunderclap, therefore indicates that the lightning strike was very near.