Using ReFH2 to Generate TUFLOW Boundary Inputs: Difference between revisions

Content deleted Content added
 
(19 intermediate revisions by 4 users not shown)
Line 1:
=Introduction=
 
Originally published in 1999, and subject to continuous development, the Flood Estimation Handbook (FEH) comprises the standard methods for estimating flood frequency. The rainfall-runoff model is one of two core handbook methods. In 2015, the Centre of Ecology and Hydrology (CEH) and Wallingford Hydro Solutions (httphttps://www.hydrosolutions.co.uk) released a new version of the Revitalised Flood Hydrograph rainfall-runoff model (ReFH2) which allows users to generate design flows and hydrographs from given rainfall events for both catchment and development sites. ReFH2 is a rainfall-runoff model specifically applicable to the UK. It takes inputs from the FEH2013 web service (https://fehweb.ceh.ac.uk), and generates design rainfall events and provides a method for calculating design runoff from sites or contributing subcatchments.
For a full description of the approaches, the reader is referred to their guidance which can be freely accessed at:-
https://www.hydrosolutions.co.uk/support/refh2_faq/refh2_literature/. The ReFH2 method is available within the ReFH2 software<br>. To use the ReFH2, the software must be installed locally and a licence must be obtained from Wallingford HydroSolutions. The ReFH2 software can be installed from httphttps://files.hydrosolutions.co.uk/refh2/latest.
<br>
 
=FEH 2013 Rainfall=
FEH2013 is athe newlatest methodDepth Duration Frequency (DDF) model for generating design rainfall hyetographs. CEH recommend the use of FEH2013, supersedingwhich supersedes the FEH1999 method. In order to generate the design rainfall, the user obtains FEH2013 design rainfall depths from the FEH2013FEH webWeb serviceService at https://fehweb.ceh.ac.uk for pre-defined return period/duration combinations. This requires a log on and user credits to purchase the data for the desired location. Data is available at a river catchment scale and as a point value. Both of these provide XML containing the rainfall depths. This is then imported into the ReFH2 software to generate hyetographs based on Flood Studies ReportsReport (FSR)/FEH approaches.
<br>
 
=ReFH2 Runoff=
The first version of ReFH was first published in 2005 by Kjeldsen ''et al.''[[#References|<sup>1</sup>]].
ReFH2 is the new method for the calculation of runoff. It hasn’t changed significantly from the original ReFH approach for which equations are publicly available, although there has been a mass balance closure improvement to the runoff model. There has however, been a change to the initial conditions, BF0 and Cini (initial baseflow and initial soil moisture, C, respectively) and there is an additional parameter, alpha. The data contained in the XML from the FEH2013 website also provides the catchment descriptors to calculate the necessary model parameters within ReFH 2 from which the runoff hydrograph is developed.
as a replacement for the original FEH rainfall-runoff method, the FSR/FEH rainfall-runoff method [[#References|<sup>2</sup>]]
. ReFH2 is the newmost methodup-to-date for the calculationimplementation of runoff. It hasn’t changed significantly from the original ReFH approachmethods for whichthe equationscalculation areof publiclyrunoff. available, although there hasImprovements beeninclude a mass balance closure improvement to the runoff model. and There has however, been a changeupdates to the initial conditions, BF0 and Cini (initial baseflow and initial soil moisture, C, respectively) and there is an additional parameter, alpha. The data contained in the XML from the FEH2013 websiteWeb Service also provides the catchment descriptors to calculate the necessary model parameters within ReFH 2 from which the runoff hydrograph is developed.
<br>
 
Line 19 ⟶ 21:
[[File:New Project.png|800px]]<br>
<br>
Use the '''‘Import from file’''' option to import the XML files. Importing the XML file will populate the parameters. The XML data is available is available in catchment data or point data format. When using the point data format, these do not have an area associated with them. Therefore, the user will need to specify the area of the plot that you are interested in (if required this can also be edited later). <br>
<br>
[[File:Point_Descriptors.png|400px]]<br>
<br>
Once an area value has been provided then, it is possible to generate the rainfall hyetographs and runoff hydrographs and apply to TUFLOW in the same manner as for catchment descriptors.
The user will then choose which country the data corresponds to. The ReFH2 programme included the development of Scotland specific algorithms to estimate the model parameters from the catchment descriptors. The choice of Scotland will mean that the alpha correction factor is not applied.<br>
<br>
[[File:Catchment_Descriptors.png|400px]]<br>
<br>
Once the parameters have been imported, and the country specified, apply the parameters and choose to move to the next page. On the next page the user can choose which rainfall model to use, FEH1999 or FEH2013. Note that CEH recommend use of the improved FEH2013 model. It’s possible to specify the design rainfall return periods of interest and ReFH2 will automatically calculate the recommended duration and suggest an appropriate timestep that meets the requirement that the duration must be an odd multiple of the time step. The recommended duration should normally be used, although both values can be edited directly to provide the duration that is required. The XML file from the FEH2013FEH Web websiteService contains the rainfall depths for a number of pre-defined return period/duration combinations. For those return period/duration combinations that are not pre-defined, ReFH2 undertakes a two-way interpolation process. ReFH2 will then generate the design rainfall hyetograph based on the rainfall depth and the FSR/FEH approach.<br>
<br>
[[File:FEH_2013_Design_Rainfall.png|400px]]<br>
<br>
On the right hand side of the above image, you can see the calculated Areal Reduction Factor and Seasonal Correction Factors which will be applied to the rainfall depth. The rainfall profile can vary depending on the season selected (summer or winter) and the seasonal correction factor and areal reduction factor are both applied to the rainfall hyetograph to obtain the correct design rainfall hyetograph.
Once the Returnreturn periods and durations have been defined then click next. This brings up the various parameters together with the rainfall hyetographs and runoff hydrographs for the various return periods. The rainfall hyetographs and runoff are available as rural and urbanised scenarios.<br>
<br>
[[File:ReFH2_Results.png|400px]]<br>
Line 66 ⟶ 68:
[[File:ReFH2 Outputs.png]]<br>
<br>
The relevant data can then be copied into the TUFLOW bc_dbase folder and referenced by the '''bc_dbase.csv''' file as appropriate (see [[Tutorial Module08Tutorial_M06|Module 86]] for an example of applying direct rainfall boundary conditions for example).
The gross design rainfall or total net rainfall can be applied to directly to the 2D domain using a 2D_RF polygon to distribute the rainfall. Multiple RF polygons can be used to spatially distribute the rainfall if required.
The total runoff (or rainfall) can be applied directly to a 2D_SA polygon, to apply the inflow to an area of the 2D mesh. There are a number of options for distributing flows in this instance, these are:-
Line 102 ⟶ 104:
<br>
 
Once the bc_base has been set up then a '''.tef''' file can be generated which populates the ARI variable above with the relevant ARI for the specific question. The '''TEF''' file also creates anewa new output folder for each return period.
 
<br>
Line 119 ⟶ 121:
=Summary=
 
This post provides instructions of how to obtain direct rainfall and inflow inputs from the ReFH2 software for use within a TUFLOW model. This requires the input of data from the FEH2013FEH websiteWeb Service and the selection of the appropriate return period/duration combinations of which the user is interested. This outputs the time-varying rainfall and total runoff (as well as runoff contributions) which can be exported for use within TUFLOW. It is also possible to use TUFLOW event files to increase efficiency when creating models for multiple return period/duration combinations. FutureA developmentReFH2 into thisTUFLOW areatool willis lookavailable tofor automatethe someQGIS ofTUFLOW thisViewer processplugin, bymore interactingdetails withcan be found on the [[QGIS_ReFH2_to_TUFLOW | QGIS ReFH2 directlyto TUFLOW]] page.
 
=References=
<sup>1</sup> T.R. Kjeldsen, E.J. Stewart, J.C. Packman, S.S. Folwell & A.C. Bayliss, 2005. Revitalisation of the FSR/FEH rainfall-runoff method. Defra R&D Technical Report FD1913/TR <br>
<sup>2</sup> Houghton-Carr, H., 1999. Restatement and application of the Flood Studies Report rainfall-runoff method, Flood Estimation Handbook Volume 4.