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21 wrz 2023 · When the soil surface is warmer than the air above the surface, there is a heat exchange from the soil to the lower atmosphere in the form of sensible heat.
4 kwi 2024 · The suggestion here is that increases in sensible heat often relate to land drying and so a reduction in the fraction of available energy that is returned to the atmosphere as latent heat.
15 maj 2018 · Sensible heat, the transfer of heat from the surface to the atmosphere without any phase change, is dependent on the temperature difference between the surface and the overlying air, on...
1 paź 2018 · Key Points. Multiple sources of remote sensing-based soil moisture and latent heat flux products are integrated via triple collocation. Global observation-based estimates of coupling strength between surface soil moisture and latent heat flux are obtained.
1 lis 2021 · Based on a bulk heat transfer parameterization of turbulent fluxes of heat in atmospheric boundary layer in the context of a linear advection–diffusion equation, a new relationship is derived linking daily mean sensible and ground heat flux.
15 lis 2020 · It describes the ability to partition the net radiation (Q N) into surface sensible (Q H) and latent (Q E) heat exchange with the overlying atmosphere, and soil heat with the subsurface (Q G) assuming no heat is stored or released within the canopy.
The sensible heat flux (H) is a significant component of the surface energy balance (SEB). Sonic anemometers simultaneously measure the turbulent fluctuations of ver- 0 tical wind (w0) and sonic temperature (T s), and are commonly used to measure H.
