A. Spatially-averaged soil moisture (m3/m3) at 5, 15 and 30 cm depths and channel outlet runoff (Q in m3/s on left hand axis). B. Latent and sensible heat flux (W/m2) at the eddy covariance tower. C. Spatially-averaged soil temperature (_C) at 5, 15 and 30 cm depths.
Templeton, RC, Vivoni ER, Méndez-Barroso LA, Pierini NA, Anderson CA, Rango A, Laliberte AS, and Scott RL. 2014. High-resolution characterization of a semiarid watershed: Implications on evapotranspiration estimates. Journal of Hydrology 509: 306-319.