Sentence examples for atmosphere transfer from inspiring English sources

The heat budget of a lake includes several major factors: net incoming solar radiation, net exchange of long-wave radiation emitted by the lake surface and the atmosphere, transfer of sensible heat at the surface interface, and latent-heat processes.

Note that a detailed description of the add-on high-temperature ambient pressure reactor system and controlled atmosphere transfer will be the subject of a separate manuscript.

For instance, climate influences the distribution of vegetation on Earth's surface (e.g., deserts exist in arid regions, forests in humid regions), but vegetation in turn influences climate by reflecting radiant energy back into the atmosphere, transferring water (and latent heat) from soil to the atmosphere, and influencing the horizontal movement of air across the land surface.

Soil-vegetation-atmosphere transfer (SVAT) models require high-resolution precipitation data which often are not available at the landscape scale where spatial-sparse data are the usual setting.

The model is satisfactorily evaluated using data acquired in the framework of SALSA and a mechanistic complex SVAT model, Simple Soil-Plant-Atmosphere Transfer (SiSPAT) model.

The results showed that the formulation of advective soil vapor transport in a soil-vegetation-atmosphere transfer continuum can affect the simulated evaporation fluxes, especially under dry condition.

The soil-vegetation-atmosphere transfer (SVAT) model WAVES was used to generate relationships between net recharge (diffuse recharge minus evapotranspiration from groundwater) and depth to water table for different combinations of climate, soil and land cover types.

To address these issues, we have assessed the variability of the soil-vegetation-atmosphere-transfer model BETHY/DLR [12] and the bio-physical process model EPIC [7] on three different meteorological input datasets and two land cover maps.

Models with a spatial resolution of kilometres and a time horizon of some years as e.g. the soil-vegetation-atmosphere-transfer (SVAT) model BETHY/DLR (Biosphere Energy Transfer Hydrology Model) [12] which can be used for regional assessments of NPP or biomass development.

Afforestation may influence precipitation patterns at local to regional scales by changing surface-atmosphere transfers of heat and moisture.

To address these issues, we have assessed the variability of the soil-vegetation-atmosphere-transfer model BETHY/DLR [ 12] and the bio-physical process model EPIC [ 7] on three different meteorological input datasets and two land cover maps.