March 13, 2018 at 10:38 am #961
During model calibration, sometimes I encounter a scenario where the slope of the calculated hydrograph increases sharply corresponding to a peak (or a very high) rainfall depth at a particular time-step in the model. This ‘peak’ rainfall causes the hydrograph to ‘jump’ and therefore deviate from the observed hydrograph. I have attached some screenshots for clarity.
This is not a major concern, since the overall shape, peak, volume, rise, and recession tend to match more-or-less at the end. However, I was wondering if there is anything I could do in RORB (while running the model or in the .catg or .stm files) to reduce the impact these ‘peak’ rainfalls have on the calculated hydrograph.
Tweaking k and CL certainly reduces the magnitude of the calculated hydrograph peak to some extent, but not significantly, and it does not eliminate the peak altogether. I have also attempted to use translations on particular reaches within the .catg file as opposed to defining reach types/lengths, even though I realise this primarily just ‘pushes’ the calculated hydrograph forwards/backwards in time.
I understand that the quality of the pluviograph and/or streamflow data could certainly be a cause. But assuming the data is reliable, then apart from that, is there anything that can be done in RORB to address this issue?
Any advice/suggestions on the matter would be greatly appreciated.
Thanks in advance.
Attachments:You must be logged in to view attached files.March 14, 2018 at 9:10 pm #965
On the face of it the modelled hydrograph plots you provide look quite sensible. In the first, the ratio of the flood peaks mirror those of the rainfall peaks, where both of these are preceded by 12 or more hours of continuous rainfall. In the second plot, the first rainfall peak is over twice the size of the second, yet the observed response is greatly dampened compared to the modelled. You would appear to have adopted a time step that is suitably short compared to the period of hydrograph rise, so that’s not a problem. You don’t state what loss model you are using but from the plot it seems that you are using a IL/CL model, and it may be that you will get better agreement from adoption of an IL/PL model (though of course that does introduce problems when using the model for design purposes). You could experiment with an IL/PL model to help satisfy yourself that the rainfall data is consistent with the observed hydrograph.
My only other suggestion is to revisit model configuration. There is very little lag between the rainfall and the hydrograph centroids, so this is either a very small catchment or an urban one (or both!). Thus it may be that you need to review the length and nature of a flowpath that may be directly connected to the catchment outlet.
Anyway, my overall impression is that there are a number of things you could look at, but there is nothing obvious here to “tweak” – your difficulties reflect some portion of the catchment that is behaving differently to your understanding, or else inconsistencies in the data.
Don’t you love hydrology?
RoryMarch 19, 2018 at 3:25 pm #969
Thank you for your response. Losses are modelled using the IL/CL model. Yes, you are correct – this is a (small) rural catchment with A<10 km2. I will try your suggestions and see if there are any improvements with regards to the hydrographs peaks.
Loving it. Thank you for your advice!
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