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• W2547682919 abstract "Soil heat flux (G) is an important component of the surface energy balance and plays an important role in the partition of sensible and latent heat fluxes from the available energy. The instantaneous daytime soil heat flux can be estimated as a fraction of net radiation (Rn). Depending on vegetation cover, soil moisture, and on the time of observation, the ratio of G to Rn is different. In order to investigate the diurnal variation of G/Rn with soil moisure for bare soil , an experiment was conducted from September to November in Beijing in 2015. Based on the observations, the relationship of G/Rn in the morning and in the afternoon was formulated, respectively, by using Rn , the maximum and the minimum land surface temperatures in the morning and in the afternoon. The validation result shows that the bias between the estimated G/Rn and the observed G/Rn are 0.014 and - 0.0235 in the morning and in the afternoon, respectively. The average RMSE between the estimated G/Rn and the observed G/Rn are 0.032 and 0.0375, respectively." @default.
• W2547682919 created "2016-11-11" @default.
• W2547682919 creator A5009953160 @default.
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• W2547682919 date "2016-07-01" @default.
• W2547682919 modified "2023-09-27" @default.
• W2547682919 title "An experimental investigation on the relationship of net radiation and soil heat flux on bare land" @default.
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• W2547682919 doi "https://doi.org/10.1109/igarss.2016.7729802" @default.
• W2547682919 hasPublicationYear "2016" @default.
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