|
![]() |
|||||||||||||||||||||||||||||||||||||
Sonification Examples
The following sounds were generated at the Space Sciences Laboratory at the University of California in Berkeley using solar wind particle data from two different satellite missions, Helios 1 and 2 and the Advanced Composition Explorer (ACE).
STEREO Sonifications Click hereHelios Flux Data Sonifications For this example, we used the Solar Energetic Particles (SEP) data from the Helios mission. The data are courtesy of the Helios spacecraft investigators and Don Reames at the Goddard Space Flight Center (GSFC). The SEP data were collected in six energy bins over several years. Both the spectrograms and sounds are sorted by Carrington Rotation** To translate this SEP data to sound, each bin at each time is assigned a musical tone. The pitch of the tone remains constant, but the amplitude varies depending on the value. Thus, certain notes within the chord are louder than others, reflecting the relative flux of the energy bins. By utilizing the data from both satellites of the Helios mission, the resulting sounds have a "stereo" effect. Click on the spectrograph* below to access sounds from several Carrington rotations. Use headphones to fully appreciate the stereo effect
ACE Flux Data Sonifications For this example, we used the Iron and Helium flux data from the ACE mission. The data are courtesy of the ACE spacecraft investigators. The composition data has eight energy bins and is collected over a period of about a month.
Definitions *A spectrogram is a time series of particle data where color is used to represent flux or intensity in the various energy ranges in which measurements are made. **A Carrington Rotation is a period of 27.3 days, representing one full rotation of the Sun as seen from the Earth. Carrington Rotation numbers are arbitrarily referenced to the time the term came into use, on November 9, 1853.\
Solar Sounds The following sounds were generated by Alexander Kosovichev at Stanford University using solar data from the Michelson Doppler Imager (MDI). The procedure he used for generating these sounds was the following: He started with doppler velocity data, averaged over the solar disk, so that only modes of low angular degree (l = 0, 1, 2) remained. Subsequent processing removed the spacecraft motion effects, instrument tuning, and some spurious points. Then Kosovichev filtered the data at about 3 mHz to select clean sound waves (and not supergranulation and instrumental noise). Finally, he interpolated over the missing data and scaled the data (speeded it up a factor 42,000 to bring it into the audible human-hearing range (kHz)).
Magnetopheric Sounds The first space weather sounds were heard as far back as the 1880s, when signals resulting from magnetospheric activity were picked up by telephone lines. Many of the emissions fall within the ELF-VLF range of the radio spectrum, at frequencies of 0.1 - 10 kHz. These "Natural Radio" sounds have been compiled by Stephen P. McGreevy. The most recent recordings are available (in MP3 format) at spaceweathersounds.com. Further magnetosphere sounds have been recorded by the PWI group for the POLAR spacecraft at the University of Iowa. A table of events and sound samples are available here. Below are the magnetosphere sounds available at the PWI site:
Auroral Kilometric Radiation (AKR) consists of intense radio emissions with a frequency of 50 - 500 kHz originating in the Earth's auroral regions. The amplitudes (volume) for AKR can change 60 - 80 dB in a matter of minutes. The occurrence of these events is correlated to auroral activity. A more detailed explanation of these events can be found at the University of Iowa's POLAR Plasma Wave Investigation (PWI) page. Below is a list of auroral sounds available at the PWI site:
A small sample of the older recordings (in .wav format) by Stephen P. McGreevy at the Space Plasma Wave Group site at the University of Iowa are listed below:
|
||||||||||||||||||||||||||||||||||||||