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In this column Im going to show how to start a traverse using state plane coordinates. Before that, lets go online to the home page of the U.S. National Geodetic Survey (NGS) and locate a software program that converts geodetic coordinates to state plane coordinates. Im doing it this way because most readers of this column have access to the Internet at home. Im not going to show all web pages leading to the software, just the pertinent parts that get us to the conversion software.
The Internet address for the NGS is www.ngs.noaa.gov. Once the home page loads, click on Products and Services, a link in a list of links along the left side of the page under the header Site Contents. Scroll down the Products and Services page and click on the link for Geodetic PC Software Programs under a bold Software header. This will take you to a page with another Geodetic PC Software Programs link; click on it as well. Scroll down the next page and click on the SPCS83 (Version 2.0) link. This will bring you to a page headlined Current directory is /pub/pcsoft/spcs83. Scroll down through the warnings until you find these three files: spcs83.doc, spcs83.exe and spcs83.for. Download these files by clicking on them.
Figure 2 is a sketch of the sample problem. There are three
stations, all established using GPS. NAD 83 geodetic coordinates for each station are
given in the figure. We will use SPCS83 to calculate the state plane coordinates for each
station.
Figure 3. State Plane Zones
Figure 3 shows zone codes for each zone of every state. In our example, the zone is New Mexico Central, zone 3002. (We only have one zone in our sample problem.)
We are now ready to traverse on the state plane grid. Looking at Figure 4, we input the latitude and longitude, on the 1983 datum, for stations Bromilow, Reilly and Wakeman. The output for each station are the northing, easting, convergence and scale factor. (We havent discussed convergence, that will be in the next, and last column, of this series.) This is what we are looking for: Inversing between each pair of coordinates gives the grid distances. Taking the coordinate differences leads to the grid azimuth. From the differences in grid azimuths we get horizontal angles. We will do all these calculations, and more, in the next column. Click here to go back to the GPS Observer menu James P. Reilly serves as head of the Department of Surveying at New Mexico State University, College of Engineering, in Las Cruces. |
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