# GPS Conversions by Lloyd Borrett (

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1 GPS Conversions by Lloyd Borrett ( There are many problems associated with locating dive sites using a GPS receiver. But first it helps if you understand the way the position is given. Coordinates Latitude and Longitude coordinates are usually given in degrees, minutes and seconds, sometimes with decimals of a second added. Many navigation receivers will give positions in degrees, minutes and decimals of a minute or as degrees, minutes and seconds. Take care which you use! It is easy to convert seconds to decimal minutes simply divide the seconds by 60. Thus if we have a latitude given as S (i.e. 38 degrees, 12 minutes, 44.7 seconds South), then we divide the 45 seconds by 60 to give.75. Thus this latitude is S (i.e. 38 degrees, minutes South). To convert decimal minutes to seconds, simply multiply them by 60. So if we have a latitude given as S (i.e. 37 degrees, 15.5 minutes South), then we multiply the.5 minutes by 60 to give 30. Thus this latitude is S (i.e. 37 degrees, 15 minutes, 30 seconds South). In passing it is worth considering what both 0.01 of a minute and a second (approx minutes) represent on the Earth's surface. One hundredth of a minute is some 18.5 metres in latitude everywhere on the Earth. However the longitudinal distance varies largest at the equator and reducing as we move towards the South or North poles. For example, it is about 12 metres in longitude in the South of England at 50 North, and some 9 metres in longitude in the North of Scotland at 60 N. Similarly, a second is 1/60 of a nautical mile and thus it is about 30 metres in latitude, but some 20 metres in longitude in the South of England or some 15 metres in longitude in the North of Scotland. OK so far? Now it s time for considering the joys of datum. Datum The idea of a datum arises because the dry part of the world is lumpy. When surveyors use a theodolite to take measurements of angles and various instruments to measure distances, they need some way of calculating the results. For small areas (for instance when setting out a supermarket building) it is fine to assume that the earth is flat. We have all done some trigonometry at school and the formulae are relatively simple. (Does anyone remember the sine and cosine rules)? Page 16

2 Now on a bigger scale, say over Australia, things get a bit more complicated. Clearly the lumpy surface of the real world is too complicated to use for calculation and the Earth is not flat so another shaped surface has to be used. Take a sphere, roughly the size of the earth. Squash it along the North/South direction and wiggle it a bit to get the best fit over Australia. Bravo! Keeping it simple, you now have a datum. Calculations on this curved surface are complicated but possible. Zones Different shaped spheroids are used over different parts of the world by various mapping agencies and they have changed over time. Because Australia is so large, our charts used different datum over different zones of the country. Zones cover a much larger area than a single page in a Street Directory and are numbered according to a world wide convention. Australia is covered by 30 zones in the Universal Transverse Mercator grid system. Each zone is referred to by: A number (49 to 56) to refer a region of longitude which is 6 degrees "wide", A letter (G, H, J, K, L) to refer to a region of latitude which is 8 degrees "high". Victoria is covered by zones 54H and 55H. Melbourne, Port Phillip Bay and all point East are in zone 55H. Within each zone a Cartesian coordinate system is used to specify a location in units of metres. The East-West coordinate is called an "Easting". It is referenced to the central meridian of longitude (i.e. 3 degrees from each boundary), where it has a value of 500,000 metres. The North-South coordinate is called a "Northing". In the Southern hemisphere the 0 value is referenced to the latitude which is 10,000,000 metres South of the equator. This means that Northings in Australia have values of several million metres. A typical set of fully specified coordinates are E , N , UTM Zone 54H, Datum GDA94. OK so far? Let s move on. GPS Datum Charts of our coastal area have always been on our own Australian Geodetic Datum as this was convenient and prior to the advent of satellite navigation systems it did not matter. However GPS is a global system and the squashed sphere that is Page 17

3 a good fit in Australia is not the best fit to the real, lumpy surface over the whole world. So a revised, squashed sphere was invented. It is known as the World Geodetic System 1984, or WGS84 for short. (Logical to call it WGS when it fits the world.) The trouble is that this squashed sphere does not match up with the old Australian Geodetic Datum and the Australian Map Grid based on it. So there is a difference in apparent position for the same point on the Earth's surface when you go from one to the other. This has caused some problems to those not familiar with the idea of applying shifts to the position displayed on the GPS received. UTM Datums and Map Grids in Australia Australia now uses the GDA94 datum (Geocentric Datum of Australia 1994) for latitude / longitude and the MGA94 map grid (Map Grid of Australia 1994) for UTM coordinates. This supersedes the AGD66 (Australian Geodetic Datum 1966) and the AMG66 map grid (Australian Map Grid 1996), and their very similar counterparts AGD84 and AMG84 which were used in some parts of Australia. The change in map grid results in UTM coordinates moving about metres to the North-East, so it is important to always specify the datum when recording or publishing UTM coordinates. GDA94 is the same as the WGS84 (World Grid System 1984) for most practical purposes. The differences are of the order of a few centimetres. For Australian GPS users this means that they should switch the datum / grid on their GPS receivers from AGD66 (Aus Geoid '66) or AGD84 (Aus Geoid '84) to use WGS84/GDA94, and replace their old topographic maps with new ones which are being updated and published with the new map grid. Then no correction to position will be necessary prior to plotting. Datum Differences It is important that if you re using charts to get dive sites locations, or obtaining locations from others, you need to consider the datum being used and adjust accordingly. Failure to do so means that you may be around 180 metres from the dive site, everything else being accurate. Let s work through an example. Say someone gave you the coordinates of a wreck as 34 08' 21" S and ' 02" E. The datum used for those coordinates was the old Australian AUS66/AUS84. But, then you use the new Australian GDA94 or World WGS84 datum on your GPS as you hunt for the site. You would be metres south and metres to the west of the wreck. In a straight line, this would make you metres south-west of the wreck. So you can see how important it is that you use the right datum when using GPS. Page 18

5 suming that no gross mistake was made, will depend on the navigation system employed. For modern work the dive site position will be good to probably 10 metres, but for old work it could be 50 to 100 metres. Many records of dive sites, wrecks etc. are based on positions reported by other divers, a sinking vessel, members of the public, fishermen etc. Often there is no way of knowing how accurate the report is (or was) and they have to be accepted at face value. So if you are recording a site, use an average of the readings. Some GPS units have an averaging feature which can be set to record a certain number of readings over a period of time. The unit then provides an average reading which should, in theory, be more accurate than one recording. If you do not have this automatic feature, you can manually record a large number of readings and later average them out mathematically. Perhaps you have found the dive site now? " If ya narced and ya know it, clap ya fins " Page 20

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