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Table of Contents - The Atmospheric Studies Group at TRC

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Section 2: Geophysical D<strong>at</strong>a Processors<br />

2.1 TERREL Terrain Preprocessor<br />

TERREL is a preprocessing program th<strong>at</strong> extracts and reform<strong>at</strong>s Digital Elev<strong>at</strong>ion Model (DEM) terrain<br />

d<strong>at</strong>a according to the options selected by the user (domain, resolution, etc.). Eleven DEM form<strong>at</strong>s are<br />

currently supported. TERREL has the ability to produce Cartesian gridded fields <strong>of</strong> terrain elev<strong>at</strong>ions or a<br />

polar grid <strong>of</strong> terrain elev<strong>at</strong>ions. For the Cartesian gridded field option, TERREL averages all <strong>of</strong> the<br />

terrain d<strong>at</strong>a points which fall within the grid cell to obtain the elev<strong>at</strong>ion assigned to the center <strong>of</strong> the userspecified<br />

grid cell. When using the polar grid option, TERREL uses the maximum terrain elev<strong>at</strong>ion in the<br />

area either from the current ring out to the next ring (user input switch - SCREEN) or halfway between<br />

adjacent rings (user input switch - NORMAL) and halfway between the adjacent radials. TERREL can<br />

produce terrain d<strong>at</strong>a files in the form<strong>at</strong>s comp<strong>at</strong>ible with the following models: CALMET, MESOPAC,<br />

NUATMOS, and ISC3. TERREL requires <strong>at</strong> least one input file and produces four output files.<br />

TERREL can first be run without any d<strong>at</strong>a files and the program will indic<strong>at</strong>e for the user the l<strong>at</strong>itude and<br />

longitude <strong>of</strong> the four corners <strong>of</strong> the area required to cover the user-specified domain. A message indic<strong>at</strong>es<br />

how many terrain d<strong>at</strong>a files <strong>of</strong> each type are required based on the domain parameters supplied by the<br />

user. This is helpful, for example, when only UTM coordin<strong>at</strong>es are known, but not the l<strong>at</strong>itude and<br />

longitude <strong>of</strong> the corners <strong>of</strong> the modeling domain. Once the appropri<strong>at</strong>e d<strong>at</strong>a files are obtained, the<br />

TERREL input file must be modified to reflect the names and types <strong>of</strong> the d<strong>at</strong>a files and TERREL must<br />

be run again to process the terrain d<strong>at</strong>a. This could be done in one run or as an iter<strong>at</strong>ive process, where<br />

intermedi<strong>at</strong>e results are stored in a binary file (e.g., TERREL.SAV) and incorpor<strong>at</strong>ed into the next<br />

TERREL run using the next set <strong>of</strong> digital terrain input d<strong>at</strong>a. <strong>The</strong> .SAV file option is helpful if the user<br />

doesn't have the available disk space to store all <strong>of</strong> the raw terrain files <strong>at</strong> once.<br />

TERREL has an input (ITHRES) which is used for quality assurance purposes. ITHRES is a whole<br />

number (%) identifying the acceptable threshold <strong>of</strong> variance from the average number <strong>of</strong> d<strong>at</strong>a points<br />

('hits') per cell. If a particular grid cell had less than ITHRES percent <strong>of</strong> the average number <strong>of</strong> d<strong>at</strong>a 'hits'<br />

per cell, a warning message is written to alert the user to check the results. If using a mix <strong>of</strong> 1-degree<br />

DEM d<strong>at</strong>a and 30 meter DEM d<strong>at</strong>a, the grid cells using the 30 meter d<strong>at</strong>a will have many more 'hits' than<br />

the 1-degree DEM grid cells. <strong>The</strong> user might want to adjust the value <strong>of</strong> ITHRES to reduce the number<br />

<strong>of</strong> warning messages written.<br />

TERREL has the option (variable PMAP) to define the gridded output fields for a number <strong>of</strong> map<br />

projections. Note th<strong>at</strong> CALMET currently supports Universal Transverse Merc<strong>at</strong>or (UTM) grid,<br />

Lambert Conformal Projection (LCC) and Tangential Transverse Merc<strong>at</strong>or (TTM). Lambert Conformal<br />

Projection should be used when the modeling domain is large, (> 300 km), because a Lambert Conformal<br />

grid accounts for the earth's curv<strong>at</strong>ure. If the LCC option is specified, TERREL uses the user-specified<br />

standard parallels (l<strong>at</strong>itudes) and reference longitude to calcul<strong>at</strong>e a "cone constant" and the east-west<br />

distance from the reference longitude. <strong>The</strong> reference longitude is the longitude <strong>at</strong> which true north and<br />

map north are defined to be the same. It also defines where x=0 in the Lambert Conformal grid. <strong>The</strong><br />

reference l<strong>at</strong>itude defines where y=0 in the Lambert Conformal grid.<br />

2-3

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