“…It is shown that for the *Address correspondence to this author at the Georgian Technical University, Institute of Cybernetics, Kostava street, 77, 0175, Tbilisi, Georgia; Tel: +99532-227-406; Fax: +99532-253-898; E-mails: jandieri@access.sanet.ge, jandieri_george@yahoo.com planetary scale wave processes, neglecting dissipation, compressibility and temperature stratification, the MHD equations of the ionosphere besides the well known hydrodynamic planetary Rossby waves contain both the slow (5 100 m s 1 ) ultra-low frequency (10 Generation of slow waves is connected with electrostatic dynamo field (wind mechanism), and generation of fast waves -with vortex electrical field and electromagnetic Ampere force. The fast electromagnetic planetary waves in the local Cartesian coordinate system ( -plane approximation) were first theoretically discovered in [6,7] and slow planetary waves in [6][7][8]. The latitudinal gradients of geomagnetic field play important role in dispersion equation of these waves.…”