Fesowola O. V. Akintoye mnis, rs, mSCgis, MSc GIS & Environment.
Email: fesowola@glogeomaticsnigeria.com.
Email: fesowola@glogeomaticsnigeria.com.
MSc (Geodesy)
Email: modupe1@hotmail.com
Email: modupe1@hotmail.com
The Minna datum, a classical (optical) reference system have
been discussed severally in the past years but still being used as basis for
the Universal Transverse Mercator grid coordinates system have been over
criticized for its various limitations. The datum was the basis of the Nigerian
National Coordinates System which is no more in use. Both the national
coordinates system and Minna datum are our joint mapping legacies upon which
our national heritage has been built. A future without the understanding of the
past and learning to overcome the limitations of the past could be dangerous.
Every nation has its mapping identity and interface for global comparison. The
surveyors in Nigeria have a rich heritage in the system and datum.
The problems with classical methods used for several legacy
datum across the globe has been resolved by breaking down national framework
into state level frameworks, carrying out state level adjustments and re-adjustments
at the national grid level. This is being further improved and strengthened by
connecting to ITRF frameworks. Just as the ITRF framework is being further
improved on, every legacy framework requires the same efforts.
The International Terrestrial Reference Framework (ITRF) which
are realized from sets of coordinates of some points located globally and are
managed by International GNSS Service (IGS) on which GNSS CORS stations are
being operated is being improved on continually due to improvement in
processing strategies, techniques, and self-consistent reprocessed solution. There are different realizations since 1988
with the current realization adopted and in use, the ITRF2008 at epoch 2005.
The coordinates or position of points derived using GNSS
data acquired in 1997, ITRF 1997 realization will differ from that in result
using ITRF 2005 and ITRF 2008 realization, not to talk of ITRF2013 which would
be adopted before the end of the year. Each new framework provides a better
understanding and capability for better determination of points on the earth.
How do we respond to the management of these changing and disparate coordinates
of positions?
It is a fact that legacy and some current geospatial data
are likely to be less accurate than what we are collecting today and this raises
the question of how to make good quality decisions when the data is so
disparate. For example the American NAD 83 and WGS 84 have the same datum but
differ by about 2 meters. The NAD 83 datum origin was built on optical
measurements like our Minna datum. It has been improved upon because every
datum must be realized, must be connected to the earth; for example to the GNSS
frameworks to improve the accuracies. A single datum can have multiple
realization and for example, NAD 83 and WGS 84 have had 4-5 realization. For
better understanding of how legacy datum can be improved and adopted for
national relevance, the NAD 83, similar to Minna datum is worth looking at.
NAD 83
- Original realization was completed in 1986, almost entirely
classical (optical) observations like the Minna datum.
For improvement, the datum has been improved on thrice
· High accuracy reference network was established
by the establishments of state by state network framework based on GNSS but
included classical stations.
·
This was followed by two national re-adjustments
of
o
2007
*
NAD 83 (NSR 2007/CORS 96) Epoch 2002.00
*
National Adjustment (GNSS only)
o
2011
*
NAD 83(2011/PA11/MA11) Epoch 2010.00 that
included a nationwide GNSS only adjustments and a realization of same for CORS
and passive stations.
According to NGS, the result is not a new datum but still
NAD 83 and the national adjustment includes 80,872 passive control stations and
5 networks.
To ascertain the changes in positional coordinates and
improvement in ITRF framework at newer epochs, The UNEC station was processed
using the Trimble Online Processing facility to reflect the disparities in the
coordinates between 2011 and 2013 using ITRF 2000, 2005 and 2008 at epochs
2000, 2005 and at epoch of data respectively.
Figure 1: Coordinates of UNEC using different ITRF
Realisation
Figure 2: Position Differences in ITRF 2000 at Epoch 1997 and
ITRF 2008 at Epoch of the data
Figure 3: Position Difference of UNEC using ITRF 2005 at
Epoch 2000 and ITRF 2008 at Epoch of data
Figure 4: Position Difference of UNEC using ITRF 2008 at
Epoch of data and ITRF 2008 at Epoch 2005
Chart 1: Chart showing 2D Positional Error for UNEC Station
using different ITRF Realisation
From above, it revealed that we can have positional error
between 0.2m and 0.5m if the current ITRF realisation and epoch of the GPS data
are not taken into consideration for our GPS base station. The error budget can
be more, depending on duration of observation, processing strategy (IGS
products http://igs.org/products),
and GNSS post-processing software (Scientific or Commercial) available for
post-processing the data.
There is need to determine the change of point coordinates
as a function of time due to plate tectonic movements. This is dependent on the
epoch at which the coordinate was determined. From figures 2, 3, and 4 it is
evident that there is a minimum of 20mm position movement due to plate
tectonics, which if not taken into account over a long period of time would
affect the quality of station coordinates. The online plate motion calculator
and the results in figures above closely agree as shown in figure 5. http://www.unavco.org/software/geodetic-utilities/plate-motion-calculator/plate-motion-calculator.html
Figure 5: Result from online plate motion calculator for
UNEC Site
The various realizations of the ITRF framework bring us
closer to precise positional measurements and fixes and better understanding of
how tectonic plates movements and velocity improves our work. It is a fact that
both legacy and new geodetic datum(s) get better over time gradually achieving
their realization. The geodetic framework that produced the Minna datum was
limited in space and technology; and therefore the need for expansion, harmonization and
connection to the GNSS grids for better accuracies.
There is a need to go back to the drawing board, revisit
previous works, re-awaken the interest of those who worked tirelessly in the
past on the growth of the datum and the NNO; and pick up our abandoned legacy
in geodesy, else all efforts by the Fajemirokuns, the Agajelus, other
researchers and recent efforts by OSGOF and NSMDA will amount to wasteful
ventures.
Every geodetic framework has been the dream and vision of a
generation, most of the realization were achieved by newer minds and
researchers in the following generations; the research and contributions to
Minna datum and the Nigerian National Coordinates System have been enormous and
fruitful so far. Just as efforts by the global community have helped in the
realization of the global datum(s) and giving us a better knowledge of the
magnitudes of the velocity and movement of the tectonic plates at global
scales; a local datum can help in providing a larger scale understanding of
tectonic plate movements. The time to work on the datum and re-design the NNO to
correct for the various errors in them is now.
The Minna datum is a dream we must realize and no one will
do it for us if we don’t make efforts and help will only come when we are seen committed
and working at it. The datum will provide indigenous framework that can be
translated at will into any required global framework. It must be realized and
connected to the earth for quality and effective use.
There has been problems over the use of different datum(s)
with the UTM in Nigeria, or cross usage of data acquired at different ITRF
realization and epochs; therefore, Surveyors and GIS professionals need to
assess coordinates of datasets that are provided by various agencies using GNSS
techniques to ascertain that there are no disparities in the coordinate
reference system used. The use of the phrase
that “coordinates are based on WGS84” is an old fashioned way of supplying
point coordinates. It is highly recommended that the realization epoch must be
stated for users of the information to determine if there is need for
transformation from one epoch to another (ftp://itrf.ensg.ign.fr/pub/itrf/WGS84.TXT).
No comments:
Post a Comment