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The accuracy of these measures can be determined using the methods described above (such as radiolocation) or by using special techniques for precisely determining the ellipsoid of the datum. Special techniques have become more accurate and efficient with advances in technology. A popular method in continental areas is laser topography combined with ground-based radiolocation (see the European and Joint Research Centre 2009) with the associated databases of flood and landslide deposit materials. The accuracy of these measurements can be as low as 1cm for fixed targets and as high as 10cm for moving targets. For further discussion of this topic we refer you to the navigation section in Eos Positioning Systems 2018 and to the special issue of Navigation in the International Journal of Navigation journal in 2006. For further information on the geometric and non-geometric characteristics of terrain, see GISGeography 2019b.
For larger antenna sizes it may be possible to detect surface dynamics, such as waves, using horizonal motion. This is sometimes of considerable interest, such as to detect tidal waves, e.g. the Mersenne waves. In many situations, however, the horizonal motion is not of considerable interest. It should be noted that the horizontal motion is in the direction of the satellite motion. Surface currents also result in horizontal motion. Such methods have been used for several years. A method introduced in recent years is the use of detected ground motion, for example to determine the longitudinal and latitudinal motion of the earth relative to the geoid. However, this method is at the moment still a relatively expensive technique. The introduction of smaller and lower cost instruments may be expected to change this situation in the near future.
tremendous progress has been made in the last decade in understanding the underlying physics and geomagnetic storms affecting geodetic positioning systems, particularly with the application of swarm and swarm ii observations to gps data (e.g. skone et al. 2004, skone & yousuf 2007 ). most of the geomagnetic activity associated with the passage of the geomagnetic storm is contained in the near-field plasma sheet, which is an important source of ionospheric perturbations. near-field ionospheric perturbations are the dominant source of error in gps and waas locations, and the effects of the near-field plasma sheet on gps positioning are well documented (e. the challenge is to minimize the loss of all the information that users already possess. in order to do so, metadata may need to be more flexible and less restrictive than in the past. for example, users may be able to represent their georeferenced location using a combination of a georeference field and a textual description of the location. this approach would allow users to include a description of the location, such as ‘my’s place’, for example, and at the same time preserve the location’s information about the methods used to determine the location, such as ‘the location was georeferenced using the spatial analyst extension of arcgis 10.5.1’ ( esri 2010a ). this approach would allow users to convey as much of the location’s information as possible, while still making it possible to search for the information using standard archival techniques. however, it is important to remember that users may need to augment their descriptions with additional information about the methods used to determine the georeference, or with additional metadata that documents how the location was determined. for example, users may need to provide additional information about the types of methods used to determine the georeference, such as a catalog number for the method, or a reference to a document that describes the method. this will allow users to search for specific types of methods (e.g. the gps method ) or to more easily find information about the methods used to determine the location. when archival information is combined with additional metadata, it can be identified and searched for by non-expert users, without the need to be highly familiar with the metadata conventions of the organization that created the information. 5ec8ef588b
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