Effect of data spatial vertical resolution on the estimation of vertical profiles of the refractive index structure constant

The vertical profile of optical turbulence is a key factor in the performance design of astronomical telescopes and adaptive optics instruments. As site-testing campaigns are extremely expensive, the selection of appropriate spatial resolution data and estimation methods is extremely important. This...

Full description

Saved in:
Bibliographic Details
Published inOptics express Vol. 31; no. 16; p. 25815
Main Authors Hu, Xiaodan, Wu, Xiaoqing, Yang, Qike, Guo, Yiming, Wang, Zhiyuan, Yan, Chong, Qiao, Zhi, Qing, Chun, Li, Xuebin, Qian, Xianmei
Format Journal Article
LanguageEnglish
Published 31.07.2023
Online AccessGet full text

Cover

Loading…
More Information
Summary:The vertical profile of optical turbulence is a key factor in the performance design of astronomical telescopes and adaptive optics instruments. As site-testing campaigns are extremely expensive, the selection of appropriate spatial resolution data and estimation methods is extremely important. This study investigated the effect of using different methods (Dewan, HMNSP99, Thorpe method) to estimate the refractive index structure constant ( C n 2 ) using different resolution data (5 m, 25 m, ERA5 data) in Huaihua, Hunan. Compared with Dewan, HMNSP99 for estimating C n 2 using 5 m and 25 m resolution data, the Thorpe method almost always shows the best performance, with R XY above 0.75 and lower RMSE and MRE between estimated and measured C n 2 . The results of C n 2 estimation using HMNSP99 at different resolution data varied widely, indicating that HMNSP99 is more sensitive to the data resolution and the temperature gradient is more sensitive to the resolution. Using ERA5 data, the two methods of estimating C n 2 using Dewan and HMNSP99 have close results. It indicates that the wind shear is the main factor when the spatial resolution of the data is reduced to a certain degree, and the contribution of temperature gradient is small in the high altitude turbulence.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:1094-4087
1094-4087
DOI:10.1364/OE.493562