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High Resolution 1:10,000 scale Mapping Strategy of Multi ... - NDMA

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to transform Cartesian coordinates to latitude and longitude.<br />

Densification <strong>of</strong> Geocentric Geodetic Datum<br />

The number <strong>of</strong> stations directly realized by the geocentric geodetic system is<br />

not enough for practical use. Worldwide there are several hundred realized stations<br />

in ITRF and about twenty stations in WGS84. Therefore it is necessary to increase<br />

the density <strong>of</strong> the local stations based on the given stations in each nation or area.<br />

Examples <strong>of</strong> densification projects are NAD83 in North America, SIRGAS in South<br />

America and ETRF in Europe.<br />

International Scenario<br />

Most <strong>of</strong> the international community is switching over to the geocentric<br />

reference system. The GRS67, GRS80, WGS84 and ITRS are results <strong>of</strong> the efforts<br />

to arrive at the best possible geocentric system. The developed countries have<br />

already defined their datum on geocentric system. Some <strong>of</strong> the developing countries<br />

are on the way <strong>of</strong> realizing their datum. At the XX General Assembly <strong>of</strong> the<br />

International Union <strong>of</strong> Geodesists and Geophysicists (IUGG) in 1992, the<br />

International Association <strong>of</strong> Geodesy (IAG) made the following recommendations in<br />

its <strong>Resolution</strong> no. 1[IAG,1992]:<br />

“1) that groups making highly accurate geodetic, geodynamic or oceanographic<br />

analysis should either use the ITRF directly or carefully tie their own systems to it”<br />

“4) that for high accuracy in continental areas, a system moving with a rigid [tectonic]<br />

plate may be used to eliminate unnecessary velocities provided it coincides exactly<br />

with the ITRS at a specific epoch,<br />

It is clear that these recommendations allows for the use <strong>of</strong> other systems<br />

providing they are carefully tied to the ITRS. It is also to be noted that in ITRF the<br />

motions <strong>of</strong> the individual tectonic plates will cause horizontal coordinates to<br />

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