inner modelling

A1 A2 A3



B1 B3 B4

B5 B6 B7

B8 B9


C1 C3 C4

C6 C7


D2 D3 D5

D6 D7 D8




Z1 Z2 Z3


The animation shows the diurnal spatio-temporal evolution of soil moisture and turbulent eddy heat flux over the Rur catchment. Since, trees have lower albedo and higher roughness coefficients, they produce higher sensible heating compared to other landcover under moist soil condition, consistent with the simulated turbulent eddy heat flux.

The simulation was done using TerrSysMP and the turbulent eddy heat flux was estimated using flux gradient relationship and averaged over an hour (30 samples per hour).

animation Z4 shrestha

Precipitation radar Uni Bonn

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