Roughness Parameter of Shallow Water Bodies

I. A. Repina; Репина И. А.; A. Yu. Artamonov; Артамонов А. Ю.; I. A. Kapustin; Капустин И. А.; A. A. Mol’kov; Мольков А. А.; V. M. Stepanenko; Степаненко В. М.

doi:10.31857/S032105962360014X

Roughness Parameter of Shallow Water Bodies

作者: Repina I.¹^,2^,3, Artamonov A.⁴, Kapustin I.⁵, Mol’kov A.⁵, Stepanenko V.⁶^,7^,8
隶属关系:
1. Obukhov Institute of Atmospheric Physics, RAS
2. Lomonosov Moscow State University, Research Computing Center
3. Moscow Center for Fundamental and Applied Mathematics
4. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, 119017, Moscow, Russia
5. Institute of Applied Physics, Russian Academy of Sciences
6. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences
7. Moscow State University, Faculty of Geography
8. Moscow State University, Research Computing Center
期: 卷 50, 编号 5 (2023)
页面: 602-612
栏目: ИССЛЕДОВАНИЯ ПРОЦЕССОВ ВЗАИМОДЕЙСТВИЯ СУШИ С АТМОСФЕРОЙ И ГИДРОЛОГИЧЕСКИХ ПОСЛЕДСТВИЙ ИЗМЕНЕНИЯ КЛИМАТА
URL: https://journals.rcsi.science/0321-0596/article/view/140801
DOI: https://doi.org/10.31857/S032105962360014X
EDN: https://elibrary.ru/KVMNHC
ID: 140801

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详细

The results of measurements of atmospheric turbulence characteristics were used to obtain parameterizations for calculating the dynamic roughness parameter and the roughness parameters for temperature and humidity for a shallow closed water body. At medium wind speeds, the results of calculations by Charnock formula are in agreement with observation data; in this case, the c parameter is three times as large as that in the case of an open ocean, and the passage from the viscous to wave mechanism occurs at high wind speeds, while the dynamic roughness parameter at the same wind speeds is greater. The roughness parameters for temperature and humidity at wind speed from 0.5 to 3 m/s are not equal. The empirical coefficients in the equations describing the ratio of the dynamic roughness to the roughness parameter for temperature (humidity) on Reynolds number are close to those obtained before for other closed water bodies, thus suggesting a common formation mechanism of transport processes in a viscous sublayer. The obtained parameterizations can be used in Earth system models and lake models for calculating turbulent flows over continental water bodies.

关键词

closed water bodies, wind waves, dynamic roughness parameter, roughness parameter for temperature and humidity, Charnock parameter

参考

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