中文摘要：

这篇论文在表面上论述研究拖系数， CD ，和理智的热流动的体积转移系数， CH ，在在西藏的 Plateau.The 的 Tanggula 通行证的永久冻土区域，数据从开路径的埃迪协变性 Systern 和 10-m 被获得在在 Qinghai-Xizang 高原(西藏的高原)上由 Cryosphere 研究车站(科学的中国学院)支持了的 TGLMS 地点的自动气象站( AWS ) .The 特征在与大气的 inst 的关系的公司和 CH

英文摘要：

This paper presents research on the surface drag coefficients, CD, and the bulk transfer coefficients of sensible heat flux, CH, in the permafrost region at the Tanggula Pass of the Tibetan Plateau. The data were obtained from the Open-Path Eddy Covariance System and the 10-m Automatic Weather Station （AWS） at the TGLMS site which supported by Cryosphere Research Station （Chinese Academy of Science） on the Qinghai-Xizang Plateau （Tibetan Plateau）. The characteristics of Co and CH in relation to atmospheric instability and wind velocity are discussed, and it was found that the bulk transfer coefficients varied with air conditions and were different in different months. However, the bulk transfer coefficients obtained from the eddy covariance system did not show a significant increasing trend with increasing atmospheric instability, and the bulk transfer coefficients did not change greatly with increasing wind velocity at 10 m.