A comparison of low-frequency radio noise amplitude probability distribution models

Citation
Da. Chrissan et Ac. Fraser-smith, A comparison of low-frequency radio noise amplitude probability distribution models, RADIO SCI, 35(1), 2000, pp. 195-208
Citations number
26
Categorie Soggetti
Earth Sciences","Eletrical & Eletronics Engineeing
Journal title
RADIO SCIENCE
ISSN journal
00486604 → ACNP
Volume
35
Issue
1
Year of publication
2000
Pages
195 - 208
Database
ISI
SICI code
0048-6604(200001/02)35:1<195:ACOLRN>2.0.ZU;2-I
Abstract
One of the most commonly modeled statistics in atmospheric radio noise stud ies is the noise envelope voltage amplitude probability distribution (APD). Although a number of models have been introduced to characterize atmospher ic noise envelope APDs, the quantity of real data that exist to verify thei r accuracy is somewhat limited, especially in the ELF and VLF bands. This p aper presents the results of a statistical analysis in which thousands of h ours of ELF/VLF noise are processed to derive APDs, which are then compared with various APD models to determine which of the models is most accurate. The error criterion used to find the optimal parameters of each APD model, as well as to compare the models against each other, is the expected value of the log error squared (where the log error is the difference in decibel s between the data histogram and the model histogram). This criterion provi des a means by which the models may be evaluated and compared numerically. The most accurate model is found to depend on geographic location, time of year and day, bandwidth, and center frequency, but two of the simplest mode ls (i.e., each with only two parameters) are found to give extremely good p erformance in general. These are the Hall and alpha-stable (or a-stable) mo dels, both of which approximate the Rayleigh distribution for low-amplitude values but decay with an inverse power law for high-amplitude values. This paper concludes that the Hall model is the optimal choice in terms of accu racy and simplicity for locations exposed to heavy sferic activity (e.g., l ower latitudes) and the alpha-stable model is best for locations relatively distant from heavy sferic activity (e.g., the polar regions).