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geographic north The direction in which the compass needle points is referred to as magnetic north, and the angle between magnetic north and the true north direction is called magnetic declination The terms variation, magnetic variation, or compass variation are often used in place of magnetic declination It is important to remember that the magnetic declination does not remain constant in time 2 What is the difference between NAD 27 and NAD 83 Geodetic datum (from Latin, singular for data, given things) de nes the reference systems that describe the size and shape of the Earth Most maps are made based on a datum (horizontal and vertical), which is the origin or reference point from which all points on a map are measured Several different datums have been used to develop maps; however, commonly used datums include the North American Datum of 1927 (NAD27), the North American Datum of 1983 (NAD83), and the World Geodetic System of 1984 (WGS84) The NAD27 is based on the Clarke ellipsoid 1866 and uses stone in Meades Ranch, Kansas as a reference point, while the NAD83 Geodetic reference system is based on satellites All North American older topographical maps are based on NAD27 3 How can I convert geographic coordinates from NAD27 to NAD83 In the US, for licensing purposes, geographic coordinates provided to the FCC via the Universal Licensing System (ULS) must be referenced to the North American Datum of 1983 (NAD83) If the source, from which the coordinates were obtained, is referenced to another datum (eg, NAD27, PRD40), they must be converted to NAD83 Mathematical models and formulas for conversion are between datums are very complex The online and downloadable tools for coordinate conversion to NAD83 can be found at http://wirelessfcc gov/uls/indexhtm job=nadcon (accessed August 25, 2009) 4 Where can I nd free detailed building and clutter data for my project The terrain data can range from a minimum terrain data, which is available for the whole world via freely available datasets (Globe, GTOPO30, SRTM), to expensive detailed building and clutter databases Even these expensive databases will be available only in areas where someone has identi ed a market opportunity suf ciently strong to justify the dataset creation costs, typically downtown areas of the major metropolitan cities.



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5 What is the consequence of referencing geodetic coordinates to the wrong geodetic datum Hundreds of different datums have been used to frame position descriptions since Aristotle made the rst estimates of the Earth size, and datums have evolved from those describing a spherical Earth to ellipsoidal models derived from years of satellite measurements Modern geodetic datums range from at-Earth models used for plane surveying to complex models used for international applications, which completely describe the size, shape, orientation, gravity eld, and angular velocity of the Earth The datum is important for Geographic Information Systems (GIS) and GPS applications to ensure consistency of map data When using a GPS receiver, the datum must be set to match the horizontal datum on the map If the datum does not match, there will be errors when plotting data on a map Referencing geodetic coordinates to the wrong datum can result in position errors of hundreds of meters or worse 6 Can I use old topographical maps for the path pro le and the microwave link design No Use updated maps not more than a year old Magnetic declination as well as the terrain itself can change signi cantly in a very short time period Make sure that everyone on the project is using the same maps, datum, and coordinate systems The datum or reference ellipsoid selection must be the same for the site data, image, and elevation les The same map projection must be used for the image and elevation les 7 Why are my GPS positions in the wrong place when I use satellite imagery In the 3-D (three-dimensional) terrain the image of the terrain is stretched over the terrain The terrain is most likely not detailed enough to be an exact match, so the photo will be stretched differently For example, Google Earth uses 30m terrain data for the US, but 90m data for most of the rest of the world So in areas of extreme topography (mountains and canyons, for example), images won t be stretched properly to t the terrain In addition, the standard elliptical WGS84 model is too simplistic, and trying to wrap data in the geographic information on such a simple model of the Earth s shape will introduce additional errors Users should not have much faith in the precision of satellite imagery for absolute positioning of objects and/or detailed path engineering.

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However, the positioning of objects relative to each other could be precisely determined; for example, the distance from the communications tower to the equipment building 8 Can we use maps instead of path surveys No Perform LOS or path surveys on all microwave links No matter how good and accurate maps are, they are only used for initial planning as a rst approximation Even if you have a very accurate (and expensive) clutter data, you may need to perform path surveys and/or establish LOS 9 What is the best resolution for the terrain elevation data that I can nd today USGS (US Geological Survey) is a multi-disciplinary science organization that focuses on biology, geography, geology, geospatial information, and water The USGS 10 Meter DEM (Digital Elevation Model) data consists of a grid of elevation values posted every 10 meters (actually, every 1/3 arc second) The USGS has released this very accurate terrain data for a large portion of the US, especially in the western states The contours produced from this data follow almost exactly the original contours from the USGS paper 1:24,000 scale Topo maps Terrain elevation data can be downloaded free of charge from The National Map Seamless Server: http://seamlessusgsgov/index php (accessed January 07, 2010) 10 Where can I nd the current value for the magnetic declination at a certain location in North America One of the possible sites providing a magnetic declination calculator is at http://geomagnrcangcca/apps/mdcal-engphp (accessed January 07, 2010)

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