Abstract
The turbulent structure parameters of temperature ( $$C_T^2$$ ) and humidity ( $$C_Q^2$$ ), and their cross-structure parameter ( $$C_{QT}$$ ), are investigated using data collected with the airborne-measurement platform Helipod during the LITFASS-2003 campaign. The flights took place within the atmospheric surface layer over heterogeneous terrain including forests, a lake and farmland. We find variability in $$C_T^2$$ along such flight legs, with values of $$C_T^2$$ over forested surfaces one order of magnitude larger than over farmland, and two orders of magnitude larger than over the lake. However, a quantitative relationship between the magnitude of $$C_Q^2$$ and the surface type is not found, most likely due to a similar surface latent heat flux between the land-use types. However, when the different flight legs are taken together and data grouped by land-use type, values of $$C_Q^2$$ are significantly lower over the lake than over the other surfaces. A classification of $$C_{QT}$$ is only possible between water and land surfaces, with lower values over water. We find the correlation coefficient $$R_{QT}$$ in the range of 0.4–1.0, which is less than unity, and thus violates the assumption of unity in Monin–Obukhov similarity theory.
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