Stellar scintillations were: measured at Mt. Maidanak during 42 nights in 1
998-1999 in order to estimate the contribution of the free atmosphere to th
e seeing. The atmosphere above 1-2 km provides a median seeing of 0".39, wh
ich is about one-third of the total seeing (0".70). The characteristic alti
tudes of turbulent layers are from 3 to 11 km above the summit, and the app
earance of layers at altitudes of 3-4 km is accompanied by a degradation of
the Free-atmosphere seeing. The median isoplanatic angle is theta (0) = 2"
.30 (lambda = 500 nm, at the zenith). This is the first time that such data
have been obtained for Maidanak.
The instruments used for these measurements-a modified four-channel photome
ter and a prototype of a double-aperture scintillation sensor-are described
in detail. The data reduction was based on accurate corrections for photon
-counting statistics and the use of theoretical weighting functions relatin
g scintillation indicts to the altitudes and intensities of turbulent layer
s. Simultaneous or quasi-simultaneous measurements of scintillation indices
using apertures of different sizes having significantly different weightin
g Functions enable estimation of the altitude and intensity of the equivale
nt turbulent layer. Despite the simplicity of this one-layer model, it prov
ides fairly robust estimates of the integrated parameters of the real free
atmosphere. (C) 2001 MAIK "Nauka/Interperiodica".