supported by the State Key Program of National Natural Science Foundation of China(41931179);the Second Tibetan Plateau Scientific Expedition and Research Program(2019QZKK020109 and 2019QZKK020611);the Major Science and Technology Project of Gansu Province(21ZD4FA010);the National Natural Science Foundation of China(11772143);the Fundamental Research Funds for the Central Universities(lzujbky2020-cd06);Scientific and Technological Research and Development Plan of China Railway Urumqi Bureau Group Co.LTD(WLMQ-KGHZGS-HRTLGGB-2020-0031);the Youth Fund of PLA Rocket Force University of Engineering(2021QN-B029)。
Atmospheric turbulence which induced by wind shear and/or convection is non-uniform anisotropic flows of high Reynolds and Rayleigh number[1].According to the mechanism of turbulence generation,atmospheric boundary-la...