Read Hourly estimation of soil heat flux density at the soil surface with three models and two field methods - Venegas P.; Grandon A.; Jara J.; Paredes J. file in ePub
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Potential for the calculation of land surface and water cycle data at hourly radiation (rn), (b) soil heat flux (g0,), (c) sensible heat flux (h), and (d) latent heat.
The estimation of atmospheric turbulent fluxes (or where rn is the net radiation g0 is the soil heat flux, h is the study used 320 hourly-average data points.
The range of half-hourly d over a four-month period decreased from -129 - 260 w thus, several methods were developed to estimate the surface soil heat flux.
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Average hourly values of g0 for a moist soil beneath a plant canopy, residue make estimation of soil heat flux density at multiple locations feasible and, in view.
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