The possibilities of reconstruction of various atmospheric structures and i
nfluence of localized atmospheric and ionospheric irregularities on the rec
onstructed atmospheric profiles are discussed. In the case of vast atmosphe
ric structures (above 400-600 km long), the radiooccultation method of atmo
spheric studies makes it possible to reconstruct the vertical profiles of m
eteorological parameters with the accuracy acceptable for applications (the
errors in the refractive index profile are 0.5-1% for the altitude region
8-40 km). However, the presence of the atmospheric irregularities with hori
zontal dimensions up to 300-400 km leads to significant reconstruction erro
rs, the fact being related to the 'spreading' of the disturbance to the ent
ire region of the sounding ray intersection of the troposphere. Therefore,
near such structures as secondary typo atmospheric fronts and developing cy
clones, the profiles are reconstructed with strong distortions reaching 1-1
0%. The impact of the irregularities in the radio signal propagation media
(atmosphere, ionosphere, and protonosphere) on the accuracy of the profiles
reconstructed is studied. Possibilities to study various atmospheric irreg
ularities by the tomographic method, using a network of ground-based receiv
ers, are considered. (C) 2001 Elsevier Science Ltd. All rights reserved.