Thermal radiation components of the energy balance at the ground

Downward atmospheric longwave irradiance under clear and cloudy skies: Measurement and parameterization

“…1992 data set for the lowland, 1993-1994 data set for the mountain site) Monteith (1961) Kew (UK) 0.53 0.065 Swinbank (1963) Australia 0.64 0.037 Sellers (1965) 22 locations World-wide 0.61 0.048 Berger et al (1984) France 0.66 0.040 Berdahl and Martin (1984) Six locations in U.S.A. 0.56 0.059 Heitor et al (1991) Lisbon ( Crawford and Duchon (1999) estimated daytime I↓ for the ARM site. In Fig.…”

Soil Temperature and Obsidian Hydration Dating: A Clarification of Variables Affecting Accuracy

“…Therefore variables such as altitude and climate modifiers which affect air temperatures should have an effect on the sensible heat flux. Another influence on the sensible heat flux is the thermal capacity of the boundary atmosphere (Monteith & Unsworth, 1990;Heitor, Biga & Rosa, 1991). So the variables of atmospheric humidity and air pressure are potentially significant.…”

Radiation Component Calculation and Energy Budget Analysis for the Korean Peninsula Region

“…DLR is longwave radiation emitted from clouds and the atmosphere that arrives at the surface. It can be calculated using its high correlation with weather variables such as the temperature near the surface and cloud information, such as total cloud cover, cloud emissivity, and cloud base temperature [66][67][68][69][70]. This study used the method presented by [71], in which DLR is calculated empirically using air temperature, total cloud cover, and water vapor pressure (Equation (16)).…”