Measured hydrometeorologic data

Solving the energy balance at the atmosphere-subsurface interface drives heat input (in the summer) into the subsurface. We use this subsequently to calculate heat transport and water flow into the subsurface and then to calculate temperature s around drinking-water supply pipes. This data is from the weather station of the University of Stuttgart. We are providing the measured Boundary Conditions, needed to compute the interface boundary conditions: long wave radiation incoming short wave radiation incoming air temperature in 2 m above ground wind velocity in 2 m above ground relative humidity in 2 m above ground precipitation intensity Data is given tabulated, a readme-file explains the column names.

解决大气-地下界面能量平衡问题，推动夏季热量向地下输入。据此，我们进一步计算地下热量传输和水流，进而计算饮用水供应管道周围的温度。此数据来源于斯图加特大学的气象站。我们提供所需计算的界面边界条件测量值：长波辐射 incoming 短波辐射 incoming 地面以上2米处的空气温度、地面以上2米处的风速、地面以上2米处的相对湿度、降水强度。数据以表格形式给出，readme文件中解释了各列名称。