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Spatial patterns in timing of the diurnal temperature cycle

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Figure

Fig. 1. Simulation of effective temperature for Ka-band emissionference (ddepths (low and deep layers are weighted equally ineffective phase difference (dfor a dry (Teff(dry)) and a wet soil Teff(wet))
Table 1. Specifications of satellite sensors providing Ka-band microwave observations used for land surface temperature estimation.
Fig. 3. Main characteristics of the diurnal temperature cycle and thedefinition of the phase of the DTC (φ).
Fig. 5. 2009 mean φ for TKa (a), TNWP (b), and TIR (c). (d) North–south transect of mean φ.
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