Differences
This shows you the differences between two versions of the page.
| Next revision | Previous revisionLast revisionBoth sides next revision | ||
| kb:modellayout [2012/07/30 22:53] – created enviadmin | kb:modellayout [2012/07/30 23:05] – enviadmin | ||
|---|---|---|---|
| Line 18: | Line 18: | ||
| Finally the **Soil Model** is need to calculate the heat transfer from the surfaces into the ground and vice versa. Also, the hydrological part of the soil model provides important information about the available water inside the soil. This data is needed to estimate the maximum transpiration of the vegetation and the available water at the soil surface. | Finally the **Soil Model** is need to calculate the heat transfer from the surfaces into the ground and vice versa. Also, the hydrological part of the soil model provides important information about the available water inside the soil. This data is needed to estimate the maximum transpiration of the vegetation and the available water at the soil surface. | ||
| + | |||
| + | ---- | ||
| + | <fs smaller> | ||
| + | **See also:** () | ||
| + | </fs> | ||
| + | ---- | ||
| + | |||
| + | |||