While some people involved in the acoustic remote sensing field are aware o
f the possibility of receiving dot echoes from nonatmospheric targets, most
of the papers available in the scientific literature dealing with this phe
nomenon associate them to atmospheric targets, such as clusters of water va
por inhomogeneity, thermodynamical processes of condensation and reevaporat
ion of water vapor, anisotropic irregularities localized in thin layers, et
c. At present, dot echoes are defined by their appearance on the echogram a
nd are nor differentiated by causative processes. As such, they share simil
ar characteristics, such as being randomly distributed and having a time le
ngth that is similar to the time length of the emitted tone. In this paper
dot echoes conforming to this definition are investigated through the analy
sis of the signal in both the time and frequency domain. The timescale of a
dot signature along with the configuration of the sodar system provide an
upper limit to the size of the targets producing these echoes. The spectral
characteristics and the first and second momenta of the echoes are compare
d with clear-air echoes as well as with echoes produced by pilot balloons r
eleased from nearby sodar antennas. The conclusion is that the dot echoes a
nalyzed in this paper are reflections from birds and are not due to atmosph
eric effects.