29 November 2016 Correlation of annual average seasonal values of temperature within the atmospheric boundary layer and amount of stratiform low clouds
Author Affiliations +
Proceedings Volume 10035, 22nd International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics; 100355N (2016) https://doi.org/10.1117/12.2248529
Event: XXII International Symposium Atmospheric and Ocean Optics. Atmospheric Physics, 2016, Tomsk, Russian Federation
Abstract
The work presents the results of the evaluation of the correlation degree of annual average seasonal temperature within the atmospheric boundary layer (at heights of 0, 400, 800, 1600 m) and the amount of low stratiform clouds (Sc, St, Ns) for the period from 1969 to 2013 performed according to the data from 6 typical weather stations of the Siberian region (Dickson, Tiksi, Salekhard, Omsk, Yakutsk, Chita). It is shown that the significant correlation (positive in winter, spring, autumn and negative in summer) between annual average seasonal values of the amount of low stratiform clouds and the temperature of the atmospheric boundary layer prevailed in Siberia during the study period. And the values of correlation coefficients (in absolute value) are more than 0.75 almost everywhere, and ones reach a maximum (0.84-0.88) at the altitude of 400 m.
© (2016) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
N. Ya. Lomakina, N. Ya. Lomakina, V. S. Komarov, V. S. Komarov, S. N. Il'in, S. N. Il'in, A. V. Lavrinenko, A. V. Lavrinenko, } "Correlation of annual average seasonal values of temperature within the atmospheric boundary layer and amount of stratiform low clouds", Proc. SPIE 10035, 22nd International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, 100355N (29 November 2016); doi: 10.1117/12.2248529; https://doi.org/10.1117/12.2248529
PROCEEDINGS
4 PAGES


SHARE
Back to Top