Environments | PYTHON :: EASI :: MODELER |
Quick links | Description :: Parameters :: Parameter descriptions :: Details :: Examples :: Algorithm :: References :: Related |
Back to top |
Back to top |
Name | Type | Caption | Length | Value range |
---|---|---|---|---|
FILE* | String | Input file name | 1 - 192 | |
DBIC* | Integer | Input raster channel or layer | 1 - 1 | |
DBOC* | Integer | Output raster channel or layer | 1 - 1 | |
BACKVAL* | Float | Background gray-level value | 1 - 1 | |
INTMETH | String | Interpolation method | 0 - 6 | CONIC | DIAG | SMOOTH Default: DIAG |
Back to top |
FILE
Specifies the PCIDSK file that contains the input and output image channels.
DBIC
Specifies the input channel storing 4-connected encoded vectors. Normally, the input layer is encoded by running GRDVEC. The input channel may be of any data type.
DBOC
Specifies the output channel in which to store the interpolated raster image. The output channel may be of any data type.
BACKVAL
Specifies the background value for the input image.
All input pixels NOT set to the background value are assumed to be encoded lines, entered by the GRDVEC function or by other means. Values are interpolated for all input pixels having the background value. BACKVAL must be of the same data type as the input channel. By default, BACKVAL is set to zero.
INTMETH
Specifies which variation of the MDIP algorithm to use for interpolation.
For more detailed information about these values, see the Algorithm section.
Back to top |
GRDINT (preceded by GRDVEC) is used to grid vector data. Gridding is the process of creating a raster image grid, given vector (line and point) data. GRDINT can interpolate (fill in) elevation data between contour lines that have been encoded into an image channel by GRDVEC. GRDVEC and GRDINT can be used to create digital elevation models (DEM).
GRDINT interpolates pixel values from an input image channel (DBIC), and saves results to an output image channel (DBOC). An interpolated value is calculated for each input pixel value that is not set to the background value (BACKVAL).
The user may choose one of three different algorithms for performing grid interpolation: diagonal search, smoothed diagonal search, or conic search; these are described in more detail in the Algorithm section.
GRDINT may be very slow for large files, especially with files containing large empty spaces, because searches are made out from each pixel of the background value until a value other than the background value is found. Completely empty images will take the most time to process.
Back to top |
The Example section of the GRDVEC documentation provides a description of how to create an elevation image (DEM) from scratch, given a topographic map with elevation contours. Normally, VECDIG, CLR, GEOSET, and GRDVEC must be run prior to running GRDINT, and a filtering function (FME or FAV) should be run on the output image from GRDINT.
GRDINT can be used to interpolate data, regardless of its source. For example, suppose we have the following 16 by 16 image, stored in a text file, gridtest.txt:
0 0 0 0 0 0 0 0 0 0 0 0 30 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 30 0 20 20 0 0 20 20 20 0 0 30 30 30 0 0 30 0 20 0 0 20 20 0 20 20 0 30 0 30 30 0 30 0 20 0 20 20 0 0 0 20 0 30 0 0 30 30 30 30 20 20 20 0 10 10 10 20 30 30 40 40 40 30 0 30 0 20 20 0 10 0 10 20 30 0 40 0 40 30 0 30 0 20 20 20 10 0 10 20 30 30 40 40 40 30 0 30 0 20 0 20 10 10 10 20 0 30 0 0 30 30 0 30 0 20 0 20 20 0 20 20 0 30 30 30 30 0 0 30 0 0 0 0 20 20 20 0 0 0 0 0 0 0 0 30 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 30 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 30 30 30 30 30 30 30 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 30 30 30 30 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 30 0 0 0 0 0 0 0 0 0
Create a 16 by 16 database file with two 8-bit channels, then run NUMREAD to read the text file and store 8-bit data in the first image channel.
EASI>FILE = "grdtest.pix" ! File name EASI>TEX1 = EASI>TEX2 = EASI>DBSZ = 16,16 ! 16 pixels by 16 lines EASI>PXSZ = 30,30 ! 30x30-meter resolution EASI>DBNC = 2,0,0,0 ! 2 8-bit channels EASI>DBLAYOUT = "PIXEL" ! Pixel interleaving EASI>RUN CIM EASI>TFILE = "gridtest.txt" EASI>NUMFORM = "DATA" EASI>DBOC = 1 EASI>MEMSIZE = EASI>DBOW = EASI>RUN NUMREAD
Perform grid interpolation of the image channel, and print the results using the NUM function. This example uses the diagonal search method.
EASI>FILE = "irvine.pix" EASI>DBIC = 1 EASI>DBOC = 2 EASI>BACKVAL = 0 ! Background value 0 EASI>INTMETH = "DIAG" ! Diagonal Search Algorithm EASI>RUN GRDINT EASI>FILE = "irvine.pix" EASI>DBIC = 2 EASI>DBIW = 0,0,16,16 ! print window 0,0,16,16 EASI>RUN NUM
NUM Database Image Numeric Window grid.pix [S 5PIC 16P 16L] 2 [ 8U] GRDINT Interpolated grid image: DBIC= 1, INTMETH=DIAG Offset: ( 0, 0) Size: ( 16, 16) 1 1 1 1 1 1 1 1 2 3 4 5 6 7 8 9 0 1 2 3 4 5 6 +--------------------------------------------------------------- 1| 20 20 20 22 22 23 24 25 24 27 28 29 26 25 24 22 2| 20 21 22 21 24 25 26 27 27 26 27 28 30 25 20 20 3| 20 20 20 20 20 23 23 30 30 30 27 28 30 25 20 20 4| 20 20 20 20 20 20 25 30 33 30 30 28 30 25 20 20 5| 20 20 15 15 15 20 25 30 35 35 30 30 30 30 20 20 6| 20 15 10 10 10 20 30 30 40 40 40 30 30 30 25 20 7| 20 15 10 10 10 20 30 35 40 40 40 30 30 30 25 20 8| 20 20 10 10 10 20 30 30 40 40 40 30 30 30 25 20 9| 20 20 10 10 10 20 25 30 35 35 30 30 30 30 25 20 10| 20 20 20 15 20 20 25 30 30 30 30 30 30 30 25 26 11| 21 22 20 20 20 26 26 27 27 28 28 29 29 30 28 27 12| 25 24 23 23 27 27 27 28 28 28 29 29 29 30 28 28 13| 27 26 26 25 25 28 28 29 29 29 29 29 29 30 30 30 14| 30 30 30 30 27 27 29 29 29 29 29 29 29 29 29 29 15| 30 29 29 30 30 30 30 29 29 29 29 29 29 29 29 29 16| 30 29 29 29 29 29 30 29 29 29 29 29 29 29 29 29
Back to top |
GRDINT uses the MDIP (Morphology-Dependent Interpolation Procedure) algorithm to calculate the gray-level value of each background (unencoded) pixel in the input image. Encoded vector data values in the input image are not changed.
The algorithm is described on pages 582-586 in the following paper:
Carrara, Alberto. "Drainage and Divide Networks Derived from High-fidelity Digital Terrain Models". Proceedings of the NATO Advanced Study Institute on Statistical Treatments for Estimation of Mineral and Energy Resources, II Ciocco (Lucca), Italy, June 22-July 4, 1986. D. Reidel Publishing Company, Dordrecht, Holland (1988). pp. 581-597.
In short, the input image around each pixel with the background value is searched in 8 directions (up, down, left, right, and four diagonals) for the location of the two nearest encoded contour lines. Each pixel is classified morphologically as residing on a slope, a depression, or a peak. The interpolation algorithm depends on this classification. The algorithm requires that contour lines be encoded into the input image using 4-connected lines, (lines are all connected by pixels in four directions, up, down, left, and right, but not along diagonals). If lines are 8-connected rather than 4-connected, the algorithm might "miss" a contour line when searching in the diagonal directions.
Back to top |
Carrara, Alberto. "Drainage and Divide Networks Derived from High-fidelity Digital Terrain Models". Proceedings of the NATO Advanced Study Institute on Statistical Treatments for Estimation of Mineral and Energy Resources, II Ciocco (Lucca), Italy, June 22-July 4, 1986. D. Reidel Publishing Company, Dordrecht, Holland (1988). pp. 581-597.
© PCI Geomatics Enterprises, Inc.®, 2024. All rights reserved.