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RouteSubSurface.c
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RouteSubSurface.c
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/*
* SUMMARY: RouteSubSurface.c - Route subsurface flow
* USAGE: Part of DHSVM
*
* AUTHOR: Bill Perkins
* ORG: PNNL
* E-MAIL: [email protected]
* ORIG-DATE: Apr-96
* DESCRIPTION: Route subsurface flow
* DESCRIP-END.
* FUNCTIONS: RouteSubSurface()
* COMMENTS:
* $Id: RouteSubSurface.c,v 1.20 2004/08/18 01:01:32 colleen Exp $
*/
#include <math.h>
#include <stdio.h>
#include <stdlib.h>
#include "settings.h"
#include "data.h"
#include "DHSVMerror.h"
#include "functions.h"
#include "constants.h"
#include "soilmoisture.h"
#include "slopeaspect.h"
#include "DHSVMChannel.h"
#ifndef MIN_GRAD
#define MIN_GRAD .3 /* minimum slope for flow to channel */
#endif
/*****************************************************************************
RouteSubSurface()
Sources:
Wigmosta, M. S., L. W. Vail, and D. P. Lettenmaier, A distributed
hydrology-vegetation model for complex terrain, Water Resour. Res.,
30(6), 1665-1679, 1994.
Quinn, P., K. Beven, P. Chevallier, and O. Planchon, The prediction of
hillslope flow paths for distributed hydrological modelling using
digital terrain models, Hydrological Processes, 5, 59-79, 1991.
This routine follows Wigmosta et al. [1994] in calculating the subsurface
flow. The local gradient is based on the local hydraulic head, consisting
of the height of the pixel surface minus the depth of the water table
below the water surface. This has the disadvantage that the local gradients
have to be recalculated for each pixel for each timestep. In Wigmosta et
al. [1994] the local gradient is taken to be equal to the slope of the land
surface, which is a reasonable assunption for mountainous areas. For the
flat boreal forest landscape it is probably better to use the slope
of the water surface.
Set the gradient with pixels that are outside tha basin to zero. This
ensures that there is no flux of water across the basin boundary. In the
current implementation water can only leave the basin as surface flow.
This may not be entirely realistic, and should be analyzed further.
One consequence of this could be that the soil in the basin is more
saturated than it would be if subsurface flow out of the basin would
be allowed.
The surrounding grid cells are numbered in the following way
|-----| DX
0-----1-----2 ---
|\ | /| |
| \ | / | |
| \ | / | | DY
| \ | / | |
| \|/ | |
7-----*-----3 ---
| /|\ |
| / | \ |
| / | \ |
| / | \ |
|/ | \|
6-----5-----4
For the current implementation it is assumed that the resolution is the
same in both the X and the Y direction. If this is not the case an error
message is generated and the program exits. The reason is that the
formulation for the flow width in the diagonal direction changes if the
grid is not square. The method for defining the flow widths in the case
of square grids is taken from Quinn et al [1991]
Update Jan 2004 COD
When Gradient = WATERTABLE, the watertable was used to route the
surface water. This was because of the common use of TopoMap.Dir and
TopoMap.TotalDir. These are now for surface routing (always) and subsurface
routing (when Gradient = TOPOGRAPHY). Subsurface routing directions
and FlowGrad (SubDir, SubTotalDir, SubFlowGrad) for Gradient = WATERTABLE
are now determined locally here (in RouteSubsurface.c.)
WORK IN PROGRESS
*****************************************************************************/
void RouteSubSurface(int Dt, MAPSIZE *Map, TOPOPIX **TopoMap,
VEGTABLE *VType, VEGPIX **VegMap,
ROADSTRUCT **Network, SOILTABLE *SType,
SOILPIX **SoilMap, CHANNEL *ChannelData,
TIMESTRUCT *Time, OPTIONSTRUCT *Options,
char *DumpPath, SEDPIX **SedMap, FINEPIX ***FineMap,
SEDTABLE *SedType, int MaxStreamID, SNOWPIX **SnowMap)
{
const char *Routine = "RouteSubSurface";
int x; /* counter */
int y; /* counter */
int i,j, ii, jj, yy, xx; /* counters for FineMap initialization */
float BankHeight;
float *Adjust;
float fract_used;
float depth;
float OutFlow;
float water_out_road;
float Transmissivity;
float AvailableWater;
int k;
float **SubFlowGrad; /* Magnitude of subsurface flow gradient
slope * width */
unsigned char ***SubDir; /* Fraction of flux moving in each direction*/
unsigned int **SubTotalDir; /* Sum of Dir array */
/* variables for mass wasting trigger. */
int count, totalcount;
float mgrid, sat;
char buffer[32];
char satoutfile[100]; /* Character arrays to hold file name. */
FILE *fs; /* File pointer. */
/*****************************************************************************
Allocate memory
****************************************************************************/
if (!(SubFlowGrad = (float **)calloc(Map->NY, sizeof(float *))))
ReportError((char *) Routine, 1);
for(i=0; i<Map->NY; i++) {
if (!(SubFlowGrad[i] = (float *)calloc(Map->NX, sizeof(float))))
ReportError((char *) Routine, 1);
}
if (!((SubDir) = (unsigned char ***) calloc(Map->NY, sizeof(unsigned char **))))
ReportError((char *) Routine, 1);
for(i=0; i<Map->NY; i++) {
if (!((SubDir)[i] = (unsigned char **) calloc(Map->NX, sizeof(unsigned char*))))
ReportError((char *) Routine, 1);
for(j=0; j<Map->NX; j++) {
if (!(SubDir[i][j] = (unsigned char *)calloc(NDIRS, sizeof(unsigned char ))))
ReportError((char *) Routine, 1);
}
}
if (!(SubTotalDir = (unsigned int **)calloc(Map->NY, sizeof(unsigned int *))))
ReportError((char *) Routine, 1);
for(i=0; i<Map->NY; i++) {
if (!(SubTotalDir[i] = (unsigned int *)calloc(Map->NX, sizeof(unsigned int))))
ReportError((char *) Routine, 1);
}
/* reset the saturated subsurface flow to zero */
for (y = 0; y < Map->NY; y++) {
for (x = 0; x < Map->NX; x++) {
if (INBASIN(TopoMap[y][x].Mask)) {
SoilMap[y][x].SatFlow = 0;
/* ChannelInt and RoadInt are initialized in Aggregate.c Why are there here? */
/* SoilMap[y][x].ChannelInt = 0; */
SoilMap[y][x].RoadInt = 0;
}
}
}
if (Options->FlowGradient == WATERTABLE)
HeadSlopeAspect(Map, TopoMap, SoilMap, SubFlowGrad, SubDir, SubTotalDir);
/* next sweep through all the grid cells, calculate the amount of
flow in each direction, and divide the flow over the surrounding
pixels */
for (y = 0; y < Map->NY; y++) {
for (x = 0; x < Map->NX; x++) {
if (INBASIN(TopoMap[y][x].Mask)) {
if (Options->FlowGradient == TOPOGRAPHY){
SubTotalDir[y][x] = TopoMap[y][x].TotalDir;
SubFlowGrad[y][x] = TopoMap[y][x].FlowGrad;
for (k = 0; k < NDIRS; k++)
SubDir[y][x][k] = TopoMap[y][x].Dir[k];
}
BankHeight = (Network[y][x].BankHeight > SoilMap[y][x].Depth) ?
SoilMap[y][x].Depth : Network[y][x].BankHeight;
Adjust = Network[y][x].Adjust;
fract_used = 0.0f;
water_out_road = 0.0;
if (!channel_grid_has_channel(ChannelData->stream_map, x, y)) {
for (k = 0; k < NDIRS; k++) {
fract_used += (float) SubDir[y][x][k];
/* fract_used += (float) TopoMap[y][x].Dir[k]; */
}
/* fract_used /= 255.0f; */
/* fract_used /= (float) TopoMap[y][x].TotalDir; */
if (SubTotalDir[y][x] > 0)
fract_used /= (float) SubTotalDir[y][x];
else
fract_used = 0.;
/* only bother calculating subsurface flow if water table is above bedrock */
if (SoilMap[y][x].TableDepth < SoilMap[y][x].Depth) {
depth =
((SoilMap[y][x].TableDepth > BankHeight) ?
SoilMap[y][x].TableDepth : BankHeight);
Transmissivity =
CalcTransmissivity(SoilMap[y][x].Depth, depth,
SType[SoilMap[y][x].Soil - 1].KsLat,
SType[SoilMap[y][x].Soil - 1].KsLatExp);
OutFlow =
(Transmissivity * fract_used * SubFlowGrad[y][x] * Dt) /
(Map->DX * Map->DY);
/* (Transmissivity * fract_used * TopoMap[y][x].FlowGrad * Dt) / */
/* (Map->DX * Map->DY); */
/* check whether enough water is available for redistribution */
AvailableWater =
CalcAvailableWater(VType[VegMap[y][x].Veg - 1].NSoilLayers,
SoilMap[y][x].Depth,
VType[VegMap[y][x].Veg - 1].RootDepth,
SType[SoilMap[y][x].Soil - 1].Porosity,
SType[SoilMap[y][x].Soil - 1].FCap,
SoilMap[y][x].TableDepth, Adjust);
OutFlow = (OutFlow > AvailableWater) ? AvailableWater : OutFlow;
}
else {
depth = SoilMap[y][x].Depth;
OutFlow = 0.0f;
}
/* compute road interception if water table is above road cut */
if (SoilMap[y][x].TableDepth < BankHeight &&
channel_grid_has_channel(ChannelData->road_map, x, y)) {
/* fract_used = ((float) Network[y][x].fraction / 255.0f); */
/* fract_used = ((float) Network[y][x].fraction / (float)TopoMap[y][x].TotalDir); */
if (SubTotalDir[y][x] > 0)
fract_used = ((float) Network[y][x].fraction /
(float)SubTotalDir[y][x]);
else
fract_used = 0.;
Transmissivity =
CalcTransmissivity(BankHeight, SoilMap[y][x].TableDepth,
SType[SoilMap[y][x].Soil - 1].KsLat,
SType[SoilMap[y][x].Soil - 1].KsLatExp);
water_out_road = (Transmissivity * fract_used *
SubFlowGrad[y][x] * Dt) / (Map->DX *
Map->DY);
/* (Transmissivity * fract_used * */
/* TopoMap[y][x].FlowGrad * Dt) / (Map->DX * */
/* Map->DY); */
AvailableWater =
CalcAvailableWater(VType[VegMap[y][x].Veg - 1].NSoilLayers,
BankHeight,
VType[VegMap[y][x].Veg - 1].RootDepth,
SType[SoilMap[y][x].Soil - 1].Porosity,
SType[SoilMap[y][x].Soil - 1].FCap,
SoilMap[y][x].TableDepth, Adjust);
water_out_road = (water_out_road > AvailableWater) ? AvailableWater
: water_out_road;
/* increase lateral inflow to road channel */
SoilMap[y][x].RoadInt = water_out_road;
channel_grid_inc_inflow(ChannelData->road_map, x, y,
water_out_road * Map->DX * Map->DY);
}
/* Subsurface Component - Decrease water change by outwater */
SoilMap[y][x].SatFlow -= OutFlow + water_out_road;
/* Assign the water to appropriate surrounding pixels */
/* OutFlow /= 255.0f; */
/* OutFlow /= (float) TopoMap[y][x].TotalDir; */
if (SubTotalDir[y][x] > 0)
OutFlow /= (float) SubTotalDir[y][x];
else
OutFlow = 0.;
for (k = 0; k < NDIRS; k++) {
int nx = xdirection[k] + x;
int ny = ydirection[k] + y;
if (valid_cell(Map, nx, ny)) {
SoilMap[ny][nx].SatFlow += OutFlow * SubDir[y][x][k];
/* SoilMap[ny][nx].SatFlow += OutFlow * TopoMap[y][x].Dir[k]; */
}
}
}
else { /* cell has a stream channel */
if (SoilMap[y][x].TableDepth < BankHeight &&
channel_grid_has_channel(ChannelData->stream_map, x, y)) {
/* float gradient = */
/* (4.0 * SoilMap[y][x].Depth > 2.0 * MIN_GRAD * Map->DX) ? */
/* 4.0 * SoilMap[y][x].Depth : 2.0 * MIN_GRAD * Map->DX; */
float gradient = 4.0 * (BankHeight - SoilMap[y][x].TableDepth);
if (gradient < 0.0)
gradient = 0.0;
Transmissivity =
CalcTransmissivity(BankHeight, SoilMap[y][x].TableDepth,
SType[SoilMap[y][x].Soil - 1].KsLat,
SType[SoilMap[y][x].Soil - 1].KsLatExp);
OutFlow = (Transmissivity * gradient * Dt) / (Map->DX * Map->DY);
/* check whether enough water is available for redistribution */
AvailableWater =
CalcAvailableWater(VType[VegMap[y][x].Veg - 1].NSoilLayers,
BankHeight,
VType[VegMap[y][x].Veg - 1].RootDepth,
SType[SoilMap[y][x].Soil - 1].Porosity,
SType[SoilMap[y][x].Soil - 1].FCap,
SoilMap[y][x].TableDepth, Adjust);
OutFlow = (OutFlow > AvailableWater) ? AvailableWater : OutFlow;
/* remove water going to channel from the grid cell */
SoilMap[y][x].SatFlow -= OutFlow;
/* contribute to channel segment lateral inflow */
channel_grid_inc_inflow(ChannelData->stream_map, x, y,
OutFlow * Map->DX * Map->DY);
SoilMap[y][x].ChannelInt += OutFlow;
}
}
}
}
}
for(i=0; i<Map->NY; i++) {
free(SubTotalDir[i]);
free(SubFlowGrad[i]);
for(j=0; j<Map->NX; j++){
free(SubDir[i][j]);
}
free(SubDir[i]);
}
free(SubDir);
free(SubTotalDir);
free(SubFlowGrad);
/**********************************************************************/
/* Dump saturation extent file to screen for Mass Wasting dates.
Saturation extent is based on the number of pixels with a water table
that is at least MTHRESH of soil depth. */
count =0;
totalcount = 0;
for (y = 0; y < Map->NY; y++) {
for (x = 0; x < Map->NX; x++) {
if (INBASIN(TopoMap[y][x].Mask)) {
mgrid = (SoilMap[y][x].Depth - SoilMap[y][x].TableDepth)/SoilMap[y][x].Depth;
if(mgrid > MTHRESH) count += 1;
totalcount +=1;
}
}
}
sat = 100.*((float)count/(float)totalcount);
sprintf(satoutfile, "%ssaturation_extent.txt", DumpPath);
if((fs=fopen(satoutfile,"a")) == NULL){
printf("Cannot open saturation extent output file.\n");
exit(0);
}
SPrintDate(&(Time->Current), buffer);
fprintf(fs, "%-20s %.4f \n", buffer, sat);
fclose(fs);
/* Initialize the mass wasting variables for all time steps
to maintain the mass balance */
if(Options->Sediment){
for (y = 0; y < Map->NY; y++) {
for (x = 0; x < Map->NX; x++) {
if (INBASIN(TopoMap[y][x].Mask)) {
for(ii=0; ii< Map->DY/Map->DMASS; ii++) { /* Fine resolution counters. */
for(jj=0; jj< Map->DX/Map->DMASS; jj++) {
yy = (int) y*Map->DY/Map->DMASS + ii;
xx = (int) x*Map->DX/Map->DMASS + jj;
(*FineMap[yy][xx]).Probability = 0.;
(*FineMap[yy][xx]).MassWasting = 0.;
(*FineMap[yy][xx]).MassDeposition = 0.;
(*FineMap[yy][xx]).SedimentToChannel = 0.;
}
}
}
}
}
/* Call the mass wasting algorithm */
if(Options->MassWaste){
if(Time->NMWMTotalSteps > 0){
if(Time->Current.Julian == Time->MWMnext.Julian){
MainMWM(SedMap, FineMap, VType, SedType, ChannelData, DumpPath, SoilMap,
Time, Map, TopoMap, SType, VegMap, MaxStreamID, SnowMap);
/* catch the next date */
for (i = 0; i < Time->NMWMTotalSteps; i++){
if(Time->MWMnext.Julian < Time->MWM[i].Julian){
Time->MWMnext = Time->MWM[i];
break;
}
}
}
}
else{ /* Time->NMWMTotalSteps == 0 run the old way*/
if((float)count/((float)totalcount) > SATPERCENT) {
MainMWM(SedMap, FineMap, VType, SedType, ChannelData, DumpPath, SoilMap,
Time, Map, TopoMap, SType, VegMap, MaxStreamID, SnowMap);
}
}
}
}
/**********************************************************************/
/* End added code. */
}