... | ... | @@ -24,6 +24,6 @@ The Scorff River data series (over 15 yrs) allowed a parameterization of these t |
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(2) for the logarithm of the flow (flow(t) in m3 /s) divided by the module of the river (5.03 m3 /s).
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For further studies simulating climate change, a temporal trend either on the mean and amplitude parameters ( *m* and *a* respectively) could be easily set up. For example, using the [river_climate_model](https://github.com/Ibasam/IBASAM/blob/master/IBASAM/R/river_climate_model.R) function and *a=3* for water temperature (i.e. increase of 3°C over 50 years) and *a=1.25* for water flow (i.e. increase of 25% of amplitude over 50 years), we obtain:
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For further studies simulating climate change, a temporal trend either on the mean and amplitude parameters ( *m* and *a* respectively) could be easily set up. For example, using the [river_climate_model](https://github.com/Ibasam/IBASAM/blob/master/IBASAM/R/river_climate_model.R) function and *m=3* for water temperature (i.e. increase of 3°C over 50 years) and *a=1.25* for water flow (i.e. increase of 25% of amplitude over 50 years), we obtain:
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![](CC.png) |
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