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Guidelines for the use of GNSS in surveying and mapping

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station need not be perfect; however, when <strong>the</strong><br />

accuracy <strong>of</strong> <strong>the</strong> height component is required to be<br />

better than 40mm, site selection is more important.<br />

In this case <strong>the</strong> reliability <strong>of</strong> <strong>the</strong> results will be<br />

adversely affected by trees block<strong>in</strong>g <strong>the</strong> signals <strong>and</strong><br />

by multipath from build<strong>in</strong>gs <strong>and</strong> reflective objects. It<br />

is best practice to select sites <strong>for</strong> <strong>GNSS</strong> control<br />

observations that have a completely clear sky view<br />

above 10° elevation <strong>and</strong> no objects such as<br />

build<strong>in</strong>gs that might ca<strong>use</strong> multipath (alternatively,<br />

Virtual RINEX data can be <strong>use</strong>d, which replaces <strong>the</strong><br />

need to set up a base station if <strong>the</strong> area is with<strong>in</strong> a<br />

COGR network). In addition, <strong>the</strong> survey stations<br />

should be connected by closed loop spirit levell<strong>in</strong>g,<br />

which should be moved up or down to best fit <strong>the</strong><br />

<strong>GNSS</strong> height observations, ra<strong>the</strong>r than adjusted to<br />

fit <strong>the</strong> <strong>GNSS</strong>-observed heights.<br />

In this section, static surveys are grouped <strong>in</strong><br />

descend<strong>in</strong>g levels <strong>of</strong> precision.<br />

4.2.1 High-precision static<br />

Dual-frequency static (<strong>for</strong> l<strong>in</strong>es <strong>of</strong> less than 100km)<br />

methods are most suitable <strong>for</strong> control surveys <strong>and</strong><br />

af<strong>for</strong>d <strong>the</strong> highest precision (sub-centimetre)<br />

achievable with <strong>GNSS</strong>. It requires <strong>the</strong> simultaneous<br />

observation at two or more stations <strong>of</strong> <strong>GNSS</strong> data<br />

from four or more common satellites. Carrier phase<br />

<strong>and</strong> code measurements are made on all available<br />

frequencies. A basel<strong>in</strong>e vector is computed after<br />

<strong>the</strong> observations have been logged, us<strong>in</strong>g a<br />

differenc<strong>in</strong>g technique. This is not expla<strong>in</strong>ed <strong>in</strong><br />

detail <strong>in</strong> this document. Full details can be found<br />

with<strong>in</strong> <strong>the</strong> books listed <strong>in</strong> Appendix C.<br />

The basel<strong>in</strong>e computation is a series <strong>of</strong> process<strong>in</strong>g<br />

steps. Triple differenc<strong>in</strong>g is <strong>of</strong>ten <strong>use</strong>d, firstly to<br />

determ<strong>in</strong>e <strong>and</strong> correct cycle slips <strong>in</strong> <strong>the</strong> data. The<br />

basel<strong>in</strong>e estimation <strong>the</strong>n proceeds us<strong>in</strong>g a double<br />

difference <strong>of</strong> <strong>the</strong> phase observables. In modern<br />

process<strong>in</strong>g methods highly advanced statistical<br />

test<strong>in</strong>g is carried out to determ<strong>in</strong>e <strong>the</strong> best<br />

c<strong>and</strong>idate with<strong>in</strong> a search area, <strong>for</strong> <strong>in</strong>teger<br />

ambiguity determ<strong>in</strong>ation. A series <strong>of</strong> solutions can<br />

be determ<strong>in</strong>ed us<strong>in</strong>g comb<strong>in</strong>ations <strong>of</strong> <strong>the</strong> phase<br />

obervables such as ‘wide lane’ or ‘narrow lane’.<br />

These are <strong>of</strong>ten <strong>use</strong>d as a step to confirm<strong>in</strong>g <strong>the</strong><br />

f<strong>in</strong>al solution, which is ei<strong>the</strong>r ‘iono free fixed’ or ‘L1<br />

fixed’, accord<strong>in</strong>g to basel<strong>in</strong>e length.<br />

A successful outcome from each <strong>of</strong> <strong>the</strong>se<br />

process<strong>in</strong>g steps is most likely when:<br />

+ <strong>the</strong>re is a large amount <strong>of</strong> good quality data<br />

+ <strong>the</strong> antennas rema<strong>in</strong> stationary dur<strong>in</strong>g <strong>the</strong><br />

observations<br />

+ <strong>the</strong>re is a significant geometry change <strong>in</strong> <strong>the</strong><br />

satellite constellation.<br />

As <strong>the</strong>se conditions all exist <strong>in</strong> <strong>the</strong> high-precision<br />

static method, <strong>the</strong> best results are achieved. The<br />

high volume <strong>of</strong> data is <strong>use</strong>d to not only solve <strong>for</strong><br />

<strong>the</strong> <strong>in</strong>teger ambiguity as mentioned above, but also<br />

to solve <strong>for</strong> o<strong>the</strong>r unknowns <strong>in</strong> <strong>the</strong> ma<strong>the</strong>matical<br />

process <strong>of</strong> comput<strong>in</strong>g <strong>the</strong> basel<strong>in</strong>e.<br />

In addition, o<strong>the</strong>r errors such as <strong>the</strong> delays ca<strong>use</strong>d<br />

by <strong>the</strong> atmospheric refraction can be solved by <strong>the</strong><br />

s<strong>of</strong>tware. In essence, high-precision surveys require<br />

<strong>the</strong> removal <strong>of</strong> as many system errors as possible.<br />

This <strong>in</strong>cludes <strong>the</strong> <strong>use</strong> <strong>of</strong> <strong>the</strong> precise ephemeris, as<br />

it removes <strong>the</strong> orbital errors which are present <strong>in</strong><br />

<strong>the</strong> broadcast ephemeris. The actual ephemeris is<br />

available <strong>in</strong> several <strong>for</strong>ms (rapid, ultra-rapid,<br />

precise) from various sites on <strong>the</strong> <strong>in</strong>ternet <strong>and</strong> is<br />

generated from earth track<strong>in</strong>g stations which<br />

precisely measure <strong>the</strong> satellite positions. It is<br />

usually available <strong>for</strong> download a few days after <strong>the</strong><br />

survey data has been logged. It is important to<br />

ensure that <strong>the</strong> make <strong>of</strong> <strong>the</strong> process<strong>in</strong>g s<strong>of</strong>tware<br />

<strong>and</strong> <strong>the</strong> version be<strong>in</strong>g <strong>use</strong>d is capable <strong>of</strong> import<strong>in</strong>g<br />

a precise ephemeris <strong>and</strong> us<strong>in</strong>g it correctly. When<br />

comput<strong>in</strong>g basel<strong>in</strong>es <strong>of</strong> longer than about 80km,<br />

‘scientific’ s<strong>of</strong>tware which <strong>in</strong>corporates algorithms<br />

to compute ocean tide load<strong>in</strong>g <strong>and</strong> tropospheric<br />

errors should be <strong>use</strong>d.<br />

Epoch sett<strong>in</strong>gs or ‘epoch <strong>in</strong>tervals’ are <strong>the</strong> rate at<br />

which data is logged <strong>in</strong> <strong>the</strong> memory <strong>of</strong> <strong>the</strong> receiver.<br />

In <strong>the</strong> differenc<strong>in</strong>g process, to compute <strong>the</strong><br />

basel<strong>in</strong>e solution <strong>the</strong> observations from one epoch<br />

are differenced with those from <strong>the</strong> next. The<br />

<strong>in</strong>terval appropriate <strong>for</strong> any particular survey<br />

depends on a variety <strong>of</strong> factors. These <strong>in</strong>clude <strong>the</strong><br />

type <strong>of</strong> basel<strong>in</strong>e process<strong>in</strong>g s<strong>of</strong>tware, <strong>the</strong> amount <strong>of</strong><br />

memory available <strong>in</strong> <strong>the</strong> receiver, <strong>and</strong> <strong>the</strong> density <strong>of</strong><br />

po<strong>in</strong>t data needed <strong>for</strong> <strong>the</strong> survey. In a static survey,<br />

as <strong>the</strong> antennas rema<strong>in</strong> fixed, <strong>the</strong>re is no need <strong>for</strong><br />

an epoch sett<strong>in</strong>g <strong>of</strong> less than 15 seconds. In some<br />

cases, when long basel<strong>in</strong>es are <strong>in</strong>volved <strong>and</strong> noisy<br />

atmospheric conditions exist, it is best to reduce<br />

<strong>the</strong> epoch sett<strong>in</strong>gs still fur<strong>the</strong>r, to 20 or 30 seconds.<br />

Whatever epoch sett<strong>in</strong>g is selected, it is imperative<br />

that all receivers <strong>use</strong>d <strong>in</strong> <strong>the</strong> survey are set to <strong>the</strong><br />

same <strong>in</strong>terval.<br />

GUIDELINES FOR THE USE OF <strong>GNSS</strong> IN LAND SURVEYING AND MAPPING |31

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