Table of Contents - The Atmospheric Studies Group at TRC

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Section 2: Geophysical Data Processors -------------------------------------------------------------------------------- INPUT GROUP: 1 -- Processing Options -------------- Intermediate data for the terrain grid are saved in a binary file for subsequent applications of TERREL. When TERREL is applied more than once (with different terrain data files), the save file must be used to pass previous results along. Previous SAVE file used to start this run (LPREV) Default: F ! LPREV = F ! T = PREV.SAV file is used F = PREV.SAV file is NOT used 2-11
Section 2: Geophysical Data Processors Table 2-2 (continued) Sample TERREL Control File Inputs (TERREL.INP) TERREL constructs gridded terrain elevations (m MSL), and may also estimate the terrain elevation at discrete points by selecting the peak elevation within a prescribed distance (km) from each point. When processing discrete points, the XYINP.DAT provides the grid coordinates (km) of each point, and may also include a height above ground (m) for each point (e.g. for elevated receptors). The structure of the XYINP.DAT file is a free-format text file with either 2 columns (X,Y) or 4 columns (X,Y,Elevation,Height). When the 4-column form is used, data in the 3rd column are replaced with the elevations obtained from the terrain data base files. Report elevations for discrete (X,Y) points (LXY) Default: F ! LXY = F ! T = Yes (XYINP.DAT and XYOUT.DAT files are used) F = No (XYINP.DAT and XYOUT.DAT files are NOT used) Interpolate elevations for discrete points (Used only if LXY=T) (LINTXY) Default: F ! LINTXY = T ! T = Yes (elevations will be interpolated) F = No (elevations will be terrain peaks) Number of data columns in XYINP.DAT file (Used only if LXY=T) (NXYCOL) Default: 4 ! NXYCOL = 2 ! Search radius (km) about each (X,Y) for locating terrain peak or for carrying out interpolation (Used only if LXY=T) (XYRADKM) No Default ! XYRADKM = 0.15 ! Some terrain data sets contain void areas where the data are missing. Others may contain areas where data are inaccurate (noisy). Both situations occur mostly over oceans or large lakes, but for SRTM data it can also occur over land due to the data set still evolving. These void (missing) or noisy input data can be replaced in several ways. Noisy Data --- Noise affects SRTM data for oceans and lakes and the adjacent shores, due to the scattering effects of water on radar measurements. The most obvious occurence of noise is negative elevations for water and adjacent land points. This can be filtered with the specification of a minimum acceptable elevation by water/land type. Extracted elevations that are greater than this minimum are retained, while those lower than this minimum value can be re-defined as missing for subsequent treatment by the missing values processing, or can be replaced with either the minimum value or with another default value defined for treatment of void (missing) data. The minimum values must be chosen judiciously for the region being treated since some regions have valid elevations below MSL. Missing data --- Cells with missing elevations can be interpolated from surrounding cells with valid values, and a maximum search radius is defined. Also, if coastline processing has been used, default elevations for each water/land type can be defined and used in place of voids. This replacement can be carried out as the final step before output on a cell-by-cell and receptor-by-receptor basis, or can be carried out for values extracted from the terrain files as missing. This 2-12
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CALPUFF Modeling System Version 6 U
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Section 1: Introduction 7.5 CALWRF
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Section 2: Geophysical Data Process
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Section 3: READ62 Upper Air Preproc
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Section 9: CALPUFF 9. CALPUFF The C
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Section 9: CALPUFF The control file
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Section 9: CALPUFF Table 9-1: Input
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Section 9: CALPUFF 9.4 Buoyant Area
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Section 9: CALPUFF 9.14 Mass Flux B
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