Abstract
In a number of studies, including our studies performed at the Institute of Atmospheric Physics, Russian Academy of Sciences, stable correlations have been found between scalar fields of the surface layer (fields of temperature and concentrations of small gas impurities—ozone and water vapor), as well as correlations between these scalars and wind speed. This article shows that the correlations of scalars can be understood on the basis of the hypothesis of similarity of surfaces with equal concentrations of impurities and isothermal surfaces, and that temperature maps explain, at a qualitative level, the correlations of temperature and speed. The unique low-inertia devices developed for pulsed measurements of the density of ozone and water vapor are described. Experiments with synchronous registration of temperature, humidity, and ozone, which showed a high correlation of the above scalar fields, and experiments with the vertically multipoint synchronous registration of temperature, which made it possible to construct maps of sections of isothermal surfaces with a vertical plane along the wind direction, are considered.
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REFERENCES
L. V. Keller and A. A. Fridman, in Proc. 1st Int. Congr. Appl. Mech., Ed. by C. B. Biezeno and J. M. Burgers (J. Waltman, Delft, 1925).
B. M. Koprov, “On the effect of thermal convection on the vertical transfer of water vapor,” Izv., Acad. Sci., USSR, Atmos. Oceanic Phys. 22 (1), 17–21 (1986).
E. K. Webb, “On the correction of flux measurements for effects of heat and water vapour transfer,” Boundary Layer Meteorol. 23 (2), 251–254 (1982).
N. F. Elansky, B. M. Koprov, D. Yu. Sokolov, and N. Thieme, “Turbulent flow of ozone over steppe,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 31 (1), 109–114 (1995).
V. I. Gorshkov and L. G. Elagina in TROPEKS-72 (Gidrometeoizdat, Leningrad, 1974), pp. 663–666 [in Russian].
Yu. A. Volkov, L. G. Elagina, and B. M. Koprov, “Spectral characteristics of the turbulent exchange between the ocean and the atmosphere in the tropical zone of the Atlantic,” Izv., Acad. Sci., USSR, Atmos. Oceanic Phys. 10 (6) 619–627 (1974).
L. G. Elagina, B. M. Koprov, and D. F. Timanovskii, “Some characteristics of the atmospheric surface layer over snow,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 14 (9), 926–931 (1978).
R. A. Antonia, A. J. Chambers, C. A. Friehe, and C. W. Van Atta, “Temperature ramps in the atmospheric surface layer,” J. Atmos. Sci. 36 (1), 99–108 (1979).
B. M. Koprov and V. M. Koprov, “On the role of vortex structures of the surface layer in the radiation interaction of the atmosphere with the underlying surface,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 56 (4), 473–481 (2020).
B. M. Koprov, V. M. Koprov, M. V. Kurgansky, and O. G. Chkhetiani, “Helicity and potential vorticity in surface turbulence,” Izv., Atmos. Oceanic Phys. 51 (6), 565–575 (2015).
B. M. Koprov, V. M. Koprov, O. A. Solenaya, O. G. Chkhetiani, and E. A. Shishov, “Technique and results of measurements of turbulent helicity in a stratified surface layer,” Izv., Atmos. Oceanic Phys. 54, 446–455 (2018).
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Koprov, B.M., Koprov, V.M. On Correlations between Fields of Temperature, Small Gas Impurities, and Wind in the Surface Layer of the Atmosphere. Izv. Atmos. Ocean. Phys. 56, 470–475 (2020). https://doi.org/10.1134/S0001433820050084
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DOI: https://doi.org/10.1134/S0001433820050084