EE-546 Wireless Communication Technologies Spring 2005 Introduction to Wireless Electromagnetic Channels & Large Scale Fading* Rahul N. Pupala
[email protected] Department of Electrical Engineering – Rutgers University, Piscataway, NJ 08854 Abstract- This article provides a brief introduction to atmosphere reflects, absorbs or scatters radio waves. wireless channels – frequency range classification of the The layers most relevant to terrestrial radio propagation electromagnetic spectra and large-scale propagation in are shown in fig 1 below. such channels. I. INTRODUCTION/MOTIVATION The term wireless communication refers to the transfer of information using electromagnetic (EM) or acoustic waves over the atmosphere rather than using any propagation medium that employs wires. Not requiring an explicit network of wires and permitting communication while on the move were the main factors which motivated the study of wireless th communication in the early 20 century. Wireless communication evolved remarkably since Fig 1: Atmospheric Layers relevant to terrestrial radio Marconi first demonstrated radio’s ability to provide propagation. continuous contact with ships sailing the English Channel in 1897. Since then, particularly during the last The troposphere is the first layer above the surface decade, the mobile radio communications industry has of the earth, and contains approximately half of the grown by orders of magnitude fueled by digital and RF earth’s atmosphere. This is the layer at which weather circuit fabrication and miniaturization techniques that takes place. The ionosphere is where ions and electrons make portable radio equipment smaller, cheaper and exist in sufficient quantities to reflect and/or refract the more reliable. Digital switching techniques have radio waves.