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Fig. 5. Time series of (a) soil temperature and heat capacity as measured by the heat pulse sensors for the 0-to 6-cm layer at the bare soil site on July 24; (b) heat storage estimated by neglecting ${partial}$ C/ ${partial}$ t (Eq. [3]), by using a constant value for heat capacity (Eq. [4]), and by including ${partial}$ C/ ${partial}$ t (Eq. [5]); and (c) cumulative heat storage for the day using the same three approaches.