Surface Layer Turbulence at the Maidanak Observatory

Author:

Azimov Azimjon1ORCID,Tillayev Yusufjon12ORCID,Ehgamberdiev Shuhrat12,Rajabov Yodgor1,Ilyasov Sabit1,Sarazin Marc3ORCID

Affiliation:

1. Ulugh Beg Astronomical Institute of the Uzbekistan Academy of Sciences, Astronomy Str. 33, Tashkent 100052, Uzbekistan

2. Department of Astronomy and Astrophysics, Physics Faculty, National University of Uzbekistan, University Str. 4, Tashkent 100174, Uzbekistan

3. European Southern Observatory, Karl-Schwarzschild-Str. 2, 85748 Garching bei München, Germany

Abstract

Results of night-time surface layer turbulence measurements using ESO LuSci at the Maidanak observatory are presented. Turbulence in the surface layer was evaluated at the Maidanak observatory using LuSci during the period of 2021–2022. The overall median DIMM-seeing was 0.74 arcseconds during this period. It was determined that the seeing in the surface layer up to 256 m equals 0.44 arcseconds. This corresponds to 42% of the contribution to the integral seeing in the entire atmosphere. A telescope installed at 6 m above the ground will be affected by 33% of the integral turbulence and about 79% of the surface layer one. Taking into account that the free atmosphere contributes around 30%, we conclude that around 30% of the overall seeing is contributed by the boundary layer above the Maidanak observatory.

Publisher

MDPI AG

Subject

Atmospheric Science,Environmental Science (miscellaneous)

Reference37 articles.

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3. Ilyasov, S., and Tillayev, Y. (2009, January 26–27). The atmospheric conditions of the Maidanak Observatory in Uzbekistan for ground-based observations. Proceedings of the International Conference on Space Information Technology, Beijing, China.

4. Seeing and atmospheric extinction at Mt. Maidanak observatory from observations with the 1.5-m AZT-22 telescope;Artamonov;Astron. Rep.,2010

5. Tillayev, Y., Azimov, A., Ehgamberdiev, S., and Ilyasov, S. (2023). Astronomical Seeing and Meteorological Parameters at Maidanak Observatory. Atmosphere, 14.

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