We present refinements for equations describing the temperature-wind covariance ($\overline{{\mathit{v}}^{\prime }{T}_a^{\prime }}$) reported by Massman and Lee (2002); namely, Eqs. (B.24), (B.25), and (B.28) in its Appendix B. The purpose of these equations is to express the wind covariance of air temperature ($T_a$) in terms of sonic temperature ($T_s$), as a sonic anemometer directly measures the latter rather than the former. Results of the derivations are summarized in Tables 1 and 2, and these refinements have been quantified using data from the Glacier Lakes Ecosystem Experiments Site (GLEES).

中文翻译：

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Massman 和 Lee (2002) 中温度-风协方差方程的改进

我们对描述温度-风协方差的方程进行了改进（$\overline{{\mathit{v}}^{‘}{吨}_A^{‘}}$) 由 Massman 和 Lee (2002) 报道；即，方程式。(B.24)、(B.25) 和 (B.28) 在其附录 B 中。这些方程的目的是表达空气温度的风协方差 (${吨}_A$) 在声波温度方面 (${吨}_{秒}$), 因为声波风速计直接测量后者而不是前者。表 1 和表 2 总结了推导结果，这些改进已使用冰川湖生态系统实验站点 (GLEES) 的数据进行了量化。