MOSAIK

Timestamp:

Mar 15, 2021 10:57:17 AM (3 years ago)

Author:

hettrich

Comment:

--

project/project/subproj/wps51

@@ -46 +46 @@
 Fig. 1 and 2 show selected results for the application of the Morris method on the horizontally homogeneous natural surface. The assessment of the relevance of the parameters can be done using the standard deviation of the output σ,,out,,. If a parameter leads to a variation of the output that corresponds to or exceeds , it can be assigned a relevance according to the prefactor z*σ,,out,,, which is shown in color in Fig. 1 c), d) and Fig. 2.
 
-[[Image(WP-S51-figure1.png)]]
+[[Image(WP_S51_figure1.png)]]
     '''Figure 1:''' Morris plots for the Morris measures with respect to the 2 m maximum (a, c) and minimum (b, d) of the potential temperature.
 ||
-[[Image(WP-S51-figure2.png)]]
+[[Image(WP_S51_figure2.png)]]
     '''Figure 2:''' Diurnal cycles of the Morris measures µ,,i,,^*^ for different inputs x,,i,, for the horizontal mean of the  2 m  potential temperature (a) and the 10 m windspeed (b).
 ||