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Commit 8e8ea84f authored by Dr. rer. nat. Jürgen Mey's avatar Dr. rer. nat. Jürgen Mey :eye:
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floodos template for flood modelling

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%--------------------------------------------------------------------------
% PREPARE GRIDS
%--------------------------------------------------------------------------
%
% addpath('.\mfiles')
% ALT (elevation model)
clear
dem=GRIDobj('./Topo/cop30DEM_utm32n_subset_carved.tif');
dem.name = 'hochrhein_subset';
% RAIN (sources (>0) and sinks (-1))
rain = dem;
rain.Z = zeros(dem.size);
% INFLOWS
inflow_rhine = 1000; % (m^3/s)
inflow_rhine_y = [63:68]; % y-location (column) of inlet
inflow_rhine_x = ones(6,1)'*286; % x-location (row) of inlet
inflow_rhine = inflow_rhine/length(inflow_rhine_x)/dem.cellsize.^2; % divide by number of inflow cells and by cellsize^2
rain.Z(inflow_rhine_y,inflow_rhine_x(1)) = ones(length(inflow_rhine_x),1)*inflow_rhine;
rain.Z(1:end,1)=-1;
rain.Z(1,1:end)=-1;
rain.Z(end,1:end)=-1;
LEM.dem = dem;
LEM.rain = rain;
GRIDobj2grd(dem,['./Topo/',dem.name,'.alt']);
GRIDobj2grd(rain,['./Topo/',dem.name,'.rain']);
%--------------------------------------------------------------------------
%% DEFINE INPUT PARAMETERS
%--------------------------------------------------------------------------
LEM.experiment = 'template'; % Project name
LEM.ErosPath = 'D:\\USER\\mey'; % Path to .exe
LEM.outfolder = 'template'; % folder to store results in
LEM.rainfall = 1; % Sets the precipitation rate per unit surface when multiplied by the rainfall map
LEM.inertia = 0; % refers to inertia term in shallow water equation
LEM.time_unit = 'year';
LEM.begin = 0; LEM.begin_option = 'time'; % start time
LEM.end = 1/365.25; LEM.end_option = 'time'; % length of model run
LEM.draw = 500; LEM.draw_option = 'time'; % output interval
LEM.step = 1; LEM.step_option = 'volume';
LEM.stepmin = 1;
LEM.stepmax = 1;
LEM.initbegin = 1e+1; % initialization time (-)
LEM.initend = 1e+1;
LEM.initstep = 2;
LEM.TU_coefficient = '1'; % sets the proportion of rain pixels that make up 1 TU
LEM.flow_model = 'stationary:pow';
LEM.erosion_multiply = 1; % multiplying factor for erosion rates. Equivalent to consider an "erosion time" larger than the hydrodynamic time
LEM.uplift_multiplier = 1;
LEM.time_extension = 1;
LEM.limiter = 1e-1;
%--------------------------------------------------------------------------
% EROSION/DEPOSITION
%--------------------------------------------------------------------------
LEM.erosion_model = 'MPM'; % (stream_power, shear_stress, shear_mpm)
LEM.deposition_model = 'constant'; % need to know whether there are other options!
LEM.eros_version = 'eros7.5.92';
LEM.stress_model = 'rgqs';
% ALLUVIAL
LEM.fluvial_stress_exponent = 1.5; % exponent in sediment flux eq. (MPM): qs = E(tau-tau_c)^a
LEM.fluvial_erodability = 2.6e-8; % [kg-1.5 m-3.5 s-2] E in MPM equation
LEM.fluvial_sediment_threshold = 0.05; % [Pa] critical shear stress (tau_c) in MPM equation
LEM.deposition_length = 30; % [m] xi in vertical erosion term: edot = qs/xi
% LATERAL EROSION/DEPOSITION
LEM.fluvial_lateral_erosion_coefficient = 1e-4; % dimensionless coefficient (Eq. 17 in Davy, Croissant, Lague (2017))
LEM.fluvial_lateral_deposition_coefficient = 0.5;
LEM.lateral_erosion_model = 1;
LEM.lateral_deposition_model = 'constant';
% BEDROCK
LEM.fluvial_basement_erodability = 0.1;
LEM.fluvial_basement_threshold = 0.5;
LEM.outbend_erosion_coefficient = 1.000000;
LEM.inbend_erosion_coefficient = 1.00000;
LEM.poisson_coefficient = 5;
LEM.diffusion_coefficient = 4;
LEM.sediment_grain = 0.0025;
LEM.basement_grain = 0.025;
%--------------------------------------------------------------------------
% FLOW MODEL
%--------------------------------------------------------------------------
LEM.friction_model = 'manning';
LEM.friction_coefficient = 0.025; %
LEM.flow_boundary = 'free';
%--------------------------------------------------------------------------
% OUTPUTS TO WRITE
%--------------------------------------------------------------------------
LEM.stress = 0;
LEM.waters = 1;
LEM.discharge = 0;
LEM.downward = 0;
LEM.slope = 0;
LEM.qs = 1;
LEM.capacity = 0;
LEM.sediment = 1;
LEM.flux =1;
LEM.stock =1;
LEM.str_write = '';
LEM.str_nowrite = '';
writeErosInputs(LEM);
%% run model
system([LEM.experiment,'.bat'])
\ No newline at end of file
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