LISFLOOD input maps for standard modules

LISFLOOD requires input files in map or text format (the latter are called tables). The detailed description is provided in this chapter of LISFLOOD User Guide.

This Annex reiterates the guidelines for the preparation of meteorological variables and provides the list of LISFLOOD input maps required when only the standard modules are used. The description of the optional modules in the OS LISFLOOD Model Documentation includes also the list of additional maps and tables.

Units of meteorological input variables

The meteorological conditions provide the driving forces behind the water balance. LISFLOOD uses the following meteorological input variables:

Code Description Unit
$P$ Precipitation $[\frac{mm}{day}]$
$ET0$ Potential (reference) evapotranspiration rate $[\frac{mm}{day}]$
$EW0$ Potential evaporation rate from open water surface $[\frac{mm}{day}]$
$ES0$ Potential evaporation rate from bare soil surface $[\frac{mm}{day}]$
$T_{avg}$ Average temperature $^\circ C$ or $K $

Both precipitation and evaporation are internally converted from intensities $[\frac{mm}{day}]$ to quantities per time step $[mm]$ by multiplying them with the time step, $\Delta t$ (in $days$). For the sake of consistency, all in- and outgoing fluxes will also be described as quantities per time step $[mm]$ in the following, unless stated otherwise.

$ET0$, $EW0$ and $ES0$ can be calculated using standard meteorological observations. LISVAP could be used for this purpose.

LISFLOOD input maps for standard modules

Table: LISFLOOD input maps.

Map Default name Units, range (indicative) Description
GENERAL      
MaskMap area.nc Unit: -
Range: 0 or 1
Boolean map that defines model boundaries
TOPOGRAPHY      
Ldd ldd.nc U.: flow directions
R.: 1 ≤ map ≤ 9
local drain direction map (with value 1-9); this file contains flow directions from each cell to its steepest downslope neighbour. Ldd directions are coded according to the following diagram:

This resembles the numeric key pad of your PC’s keyboard, except for the value 5, which defines a cell without local drain direction (pit). The pit cell at the end of the path is the outlet point of a catchment.
Grad gradient.nc U.: $\frac{m}{m}$
R.: map > 0
Slope gradient
Elevation Stdev elvstd.nc U.: $m$
R.: map ≥ 0
Standard deviation of elevation
LAND USE – fraction maps      
Fraction of water fracwater.nc U.: [-]
R.: 0 ≤ map ≤ 1
Fraction of inland water for each cell. Values range from 0 (no water at all) to 1 (pixel is 100% water)
Fraction of sealed surface fracsealed.nc U.: [-]
R.: 0 ≤ map ≤ 1
Fraction of impermeable surface for each cell. Values range from 0 (100% permeable surface – no urban at all) to 1 (100% impermeable surface).
Fraction of forest fracforest.nc U.:[-]
R.: 0 ≤ map ≤ 1
Forest fraction for each cell. Values range from 0 (no forest at all) to 1 (pixel is 100% forest)
Fraction of irrigated areas fracirrigation.nc U.:[-]
R.: 0 ≤ map ≤ 1
Irrigated fraction for each cell. Values range from 0 to 1
Fraction of rice fields fracrice.nc U.:[-]
R.: 0 ≤ map ≤ 1
Fraction for each cell dedicated to paddy rice crops. Values range from 0 to 1
Fraction of other land cover fracother.nc U.: [-]
R.: 0 ≤ map ≤ 1
Other (non-forested natural area, pervious surface of urban areas, shrubs abd bushes, …) fraction for each cell.
LAND COVER depending maps      
Crop coeff. for forest cropcoef_forest.nc U.: [-]
R.: 0.2≤ map ≤ 1.2
Crop coefficient for forest
Crop coeff. for other cropcoef_other.nc U.: [-]
R.: 0.2≤ map ≤ 1.2
Crop coefficient for other
Crop coeff. for irrigated areas cropcoef_irr.nc U.: [-]
R.: 0.2≤ map ≤ 1.2
Crop coefficient for irrigated areas
Crop group number for forest crgrnum_forest.nc U.: [-]
R.: 1 ≤ map ≤ 5
Crop group number for forest
Crop group number for forest crgrnum_other.nc U.: [-]
R.: 1 ≤ map ≤ 5
Crop group number for other
Crop group number for irrigated areas crgrnum_irr.nc U.: [-]
R.: 1 ≤ map ≤ 5
Crop group number for irrigation
Manning for forest mannings_forest.nc U.: $m^{1/3} s^{-1}$
R.: 0.015≤ map ≤ 0.4
Manning’s roughness for forest
Manning for other mannings_other.nc U.: $m^{1/3} s^{-1}$
R.: 0.015≤ map ≤0.4
Manning’s roughness for other
Manning for irrigation mannings_irr.nc U.: $m^{1/3} s^{-1}$
R.: 0.015≤ map ≤0.4
Manning’s roughness for irrigation
Soil depth for forest for layer1 soildepth1_forest.nc U.: $mm$
R.: map ≥ 50
Forest soil depth for soil layer 1
Soil depth for other for layer1 soildepth1_other.nc U.: $mm$
R.: map ≥ 50
Other soil depth for soil layer 1
Soil depth for forest for layer2 soildepth2_forest.nc U.: $mm$
R.: map ≥ 50
Forest soil depth for soil layer 2
Soil depth for other for layer2 soildepth2_other.nc U.: $mm$
R.: map ≥ 50
Other soil soil depth for soil layer 2
Soil depth for forest for layer3 soildepth3_forest.nc U.: $mm$
R.: map ≥ 50
Forest soil depth for soil layer 3
Soil depth for other for layer3 soildepth3_other.nc U.: $mm$
R.: map ≥ 50
Other soil soil depth for soil layer 3
SOIL HYDRAULIC PROPERTIES (depending on soil texture)      
ThetaSat1 for forest thetas1_forest.nc U.: [V/V]
R.: 0 < map < 1
Saturated volumetric soil moisture content layer 1
ThetaSat1 for other thetas1_other.nc U.: [V/V]
R.: 0 < map < 1
Saturated volumetric soil moisture content layer 1
ThetaSat2 for forest thetas2_forest.nc U.: [V/V]
R.: 0 < map < 1
Saturated volumetric soil moisture content layer 2
ThetaSat2 for other thetas2_other.nc U.: [V/V]
R.: 0 < map < 1
Saturated volumetric soil moisture content layer 2
ThetaSat3 for forest and other thetas2.nc U.: [V/V]
R.: 0 < map < 1
Saturated volumetric soil moisture content layer 3
ThetaRes1 for forest thetar1_forest.nc U.: [V/V]
R.: 0 < map < 1
Residual volumetric soil moisture content layer 1
ThetaRes1 for other thetar1_other.nc U.: [V/V]
R.: 0 < map < 1
Residual volumetric soil moisture content layer 1
ThetaRes2 for forest thetar2_forest.nc U.: [V/V]
R.: 0 < map < 1
Residual volumetric soil moisture content layer 2
ThetaRes2 for other thetar2_other.nc U.: [V/V]
R.: 0 < map < 1
Residual volumetric soil moisture content layer 2
ThetaRes3 for forest and other thetar2.nc U.: [V/V]
R.: 0 < map < 1
Residual volumetric soil moisture content layer 3
Lambda1 for forest lambda1_forest.nc U.: [-]
R.: map>0
Pore size index (λ) layer 1
Lambda1 for other lambda1_other.nc U.: [-]
R.: map>0
Pore size index (λ) layer 1
Lambda2 for forest lambda2_forest.nc U.: [-]
R.: map>0
Pore size index (λ) layer 2
Lambda2 for other lambda2_other.nc U.: [-]
R.: map>0
Pore size index (λ) layer 2
Lambda3 for forest and other lambda2.nc U.: [-]
R.: map>0
Pore size index (λ) layer 3
GenuAlpha1 for forest alpha1_forest.nc U.: $\frac{1} {cm}$
R.: 0 < map < 1
Van Genuchten parameter α layer 1
GenuAlpha1 for other alpha1_other.nc U.: $\frac{1} {cm}$
R.: 0 < map < 1
Van Genuchten parameter α layer 1
GenuAlpha2 for forest alpha2_forest.nc U.: $\frac{1} {cm}$
R.: 0 < map < 1
Van Genuchten parameter α layer 2
GenuAlpha2 for other alpha2_other.nc U.: $\frac{1} {cm}$
R.: 0 < map < 1
Van Genuchten parameter α layer 2
GenuAlpha3 for forest and other alpha2.nc U.: $\frac{1} {cm}$
R.: 0 < map < 1
Van Genuchten parameter α layer 3
KSat1 for forest ksat1_forest.nc U.: $\frac{mm} {day}$
R.: map>0
Saturated conductivity layer 1
KSat1 for other ksat1_other.nc U.: $\frac{mm} {day}$
R.: map>0
Saturated conductivity layer 1
KSat2 for forest ksat2_forest.nc U.: $\frac{mm} {day}$
R.: map>0
Saturated conductivity layer 2
KSat2 for other ksat2_other.nc U.: $\frac{mm} {day}$
R.: map>0
Saturated conductivity layer 2
KSat3 for forest and other ksat3.nc U.: $\frac{mm} {day}$
R.: map>0
Saturated conductivity layer 3
CHANNEL GEOMETRY      
Channels chan.nc U.: [-]
R.: 0 or 1
Map with Boolean 1 for all channel pixels, and Boolean 0 for all other pixels on MaskMap
ChanGrad changrad.nc U.: $\frac{m} {m}$
R.: map > 0
!!!
Channel gradient
ChanMan chanman.nc U.: $m^{-1/3} s$
R.: map > 0
Manning’s roughness coefficient for channels
ChanLength chanleng.nc U.: $m$
R.: map > 0
Channel length (can exceed grid size, to account for meandering rivers)
ChanBottomWidth chanbw.nc U.: $m$
R.: map > 0
Channel bottom width
ChanSdXdY chans.nc U.: $\frac{m} {m}$
R.: map ≥ 0
Channel side slope Important: defined as horizontal divided by vertical distance (dx/dy); this may be confusing because slope is usually defined the other way round (i.e. dy/dx)!
ChanDepthThreshold chanbnkf.nc U.: $m$
R.: map > 0
Bankfull channel depth
METEOROLOGICAL VARIABLES      
PrecipitationMaps pr U.: $\frac{mm} {day}$
R.: map ≥ 0
Precipitation rate
TavgMaps ta U.: $°C$
R.:-50 ≤map ≤ +50 or U.: $K$
Average temperature
E0Maps e U.: $\frac{mm} {day}$
R.: map ≥ 0
Daily potential evaporation rate, free water surface
ES0Maps es U.: $\frac{mm} {day}$
R.: map ≥ 0
Daily potential evaporation rate, bare soil
ET0Maps et U.: $\frac{mm} {day}$
R.: map ≥ 0
Daily potential evapotranspiration rate, reference crop
DEVELOPMENT OF VEGETATION OVER TIME      
LAIMaps for forest lai_forest U.: $\frac{m^2} {m^2}$
R.: map ≥ 0
Pixel-average Leaf Area Index for forest
LAIMaps for other lai_other U.: $\frac{m^2} {m^2}$
R.: map ≥ 0
Pixel-average Leaf Area Index for other
LAIMaps for irrigation lai_irrigation U.: $\frac{m^2} {m^2}$
R.: map ≥ 0
Pixel-average Leaf Area Index for irrigated areas
DEFINITION OF INPUT/OUTPUT TIMESERIES      
Gauges outlets.nc U.: [-]
R.: For each station an individual number
Nominal map with locations at which discharge timeseries are reported (usually correspond to gauging stations)

Table: Maps that define grid size, always required when using geographic (lat/lon) coordinate system.*

Map Default name Units, range Description
PixelLengthUser pixleng.nc U.: $m$
R.: map > 0
Map with pixel length
PixelAreaUser pixarea.nc U.: $m$
R.: map > 0
Map with pixel area

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