Abstract
The second part of the paper is devoted to the analysis of how heights of intense turbulent exchange and their corresponding temperature gradients in the atmospheric boundary layer are interrelated with ground values of the wind velocity and vertical turbulent heat flow. We consider only cases of temperature inversions in winter (January–February 2020). The division of inversions into two types (ground and raised) and four forms is introduced and the statistic for the height of the turbulent exchange region is obtained for them. According to results of the analysis, a conclusion is made that the direct (well-defined) relation between the height of the intense turbulent heat exchange layer and ground values of the wind velocity and turbulent heat flow is absent under conditions of temperature inversions.
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ACKNOWLEDGMENTS
The experimental data were obtained using the instrumentation of the “Atmosphere” Common Use Center of the Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences.
Funding
Atmosphere characteristics were measured with financial support from the Russian Science Foundation (project no. 19-71-20042). The development of methodical aspects of the performed investigations was supported by the Ministry of Science and Higher Education of the Russian Federation.
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Translated by A. Nikol’skii
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Odintsov, S.L., Gladkikh, V.A., Kamardin, A.P. et al. Height of the Region of Intense Turbulent Heat Exchange in a Stably Stratified Boundary Layer of the Atmosphere. Part 2: Relationship with Surface Meteorological Parameters. Atmos Ocean Opt 34, 117–127 (2021). https://doi.org/10.1134/S1024856021020068
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DOI: https://doi.org/10.1134/S1024856021020068