scholarly journals Determination of the Structural Characteristic of the Refractive Index of Optical Waves in the Atmospheric Boundary Layer with Remote Acoustic Sounding Facilities

Atmosphere ◽  
2019 ◽  
Vol 10 (11) ◽  
pp. 711 ◽  
Author(s):  
Odintsov ◽  
Gladkikh ◽  
Kamardin ◽  
Nevzorova

The structural characteristic of the refractive index of optical waves was calculated from experimental data on the microstructure of the temperature turbulence in the atmospheric boundary layer. The experimental data were obtained with an acoustic meteorological radar (sodar), ultrasonic anemometer–thermometer, and meteorological temperature profilometer. Estimates of the structural characteristics for different conditions in the atmospheric boundary layer are presented and were compared with model profiles.

2018 ◽  
Vol 31 (5) ◽  
pp. 445-450 ◽  
Author(s):  
S. L. Odintsov ◽  
V. A. Gladkikh ◽  
A. P. Kamardin ◽  
V. P. Mamyshev ◽  
I. V. Nevzorova

2018 ◽  
Vol 31 (5) ◽  
pp. 437-444 ◽  
Author(s):  
S. L. Odintsov ◽  
V. A. Gladkikh ◽  
A. P. Kamardin ◽  
V. P. Mamyshev ◽  
I. V. Nevzorova

Author(s):  
O. G. Chkhetiani ◽  
N. V. Vazaeva

A simple model for the development of submesoscale perturbations in the atmospheric boundary layer (ABL) is proposed. The growth of perturbations is associated with the shear algebraic instability of the wind velocity profile in the atmospheric boundary layer (ABL). For the scales of optimal perturbations (streaks) in the lower part of the ABL, estimates of their sizes were obtained about 100-200 m vertically and 300-600 m horizontally. Similar scales are noted for experimental data on the structure of the wind field in the lower part of the ABL, obtained in 2017, 2018 in the summer at the Tsimlyansk Scientific Station at the acoustic sounding of the atmosphere by the Doppler three-component minisodar of high resolution.


2017 ◽  
Vol 30 (10) ◽  
pp. 821-828
Author(s):  
S.L. Odintsov ◽  
V.A. Gladkikh ◽  
A.P. Kamardin ◽  
V.P. Mamyshev ◽  
I.V. Nevzorova

1989 ◽  
Vol 1 (4) ◽  
pp. 363-372 ◽  
Author(s):  
Alistair D. Culf

The records obtained from a monostatic acoustic sounder run at Halley, Antarctica, have been analysed with the use of data from instruments on a 32 m mast and from radiosonde ascents. Echoes representing ground-based layers, waves, and shallow gravity currents are discussed. The spiky ground-based echo is related to a westerly surface wind, whilst a layered wavy flow is related to surface easterlies. Such relationships are consistent with the sloped inversion wind regime at Halley.


1979 ◽  
Vol 17 (2) ◽  
pp. 223-230 ◽  
Author(s):  
T. J. Moulsley ◽  
R. S. Cole ◽  
D. N. Asimakopoulos ◽  
S. J. Caughey

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