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Kathmandu University
Department of Geomatics Engineering
Presenter
A PRESENTATION ON PREPARATION OF DEFORMATION
MODEL OF CENTRAL NEPAL DUE TO GORKHA
EARTHQUAKE 2015 AND THE AFTERSHOCK
Ashmita Dhakal | Rohit Gautam | Aakash Thapa | Prashant Thapaliya
Kathmandu University
Department of Geomatics Engineering
2
9/18/2019
INTRODUCTION
o On April 25, 2015, Gorkha earthquake of 7.8 moment magnitude
occurred causing death of around 9,000 people.
o Thousands were injured and more than 6 lakhs structures in
Kathmandu were damaged or destroyed.
o On May 12,2015, aftershock of 7.3 Mw struck in Dolakha killing
more than 100 people.
o Compressional pressure between Eurasian tectonic plate and
Indian section of Indo-Australian Plate; subducts the Eurasian
Plate (Rafferty, 2019).
o Deformation of surface
o CORS
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PROBLEM STATEMENT
o No revision and update of control points in Nepal.
o No significant steps taken by authority to calculate
deformation.
o Existing maps prepared by Survey Department long time
ago need to be updated.
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Department of Geomatics Engineering
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OBJECTIVES
Primary Objective
Prepare deformation model
of central Nepal due to
Gorkha Earthquake 2015
and the aftershock.
Secondary Objectives
To determine northing,
easting and vertical shift of
each station.
To interpolate the
deformation on ground
between the stations.
To visualize result in web
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5
Bounding box:
• 2985496.754 m
to 3190768.567
m in northing
• 182112.662 m
to 471679.824
m in easting
STUDY AREA
Figure: Map of Nepal showing the study area
Area- 42000 sq. km
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Department of Geomatics Engineering
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DATA SOURCES
UNAVCO (UNAVCO, 2019)
To download data of CORS
ITRF
(International Terrestrial Reference Frame, 2016)
To obtain the coordinates of base station
for post processing
GNSS Calendar (Jahic, 2016)
To download SP3 files
NEVADA Geodetic Laboratory
(Nevada Geodetic Laboratory, 2019)
To compare the shift computed with the
shift available in the website
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SOFTWARE USED
Satlab Geobitz
Solutions
To post-processing
data in RINEX to
produce more
accurate result
ArcGIS
To interpolate,
visualization and
map layout
MS Office
Packages
Microsoft Excel for
data manipulation,
analysis, management
and calculation and
MS Word to prepare
the report
Visual Studio
Code
To write codes for
web app
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Department of Geomatics Engineering9/18/2019
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No
Yes
Validated Coordinates with ITRF Coordinate of 2016
Post Processing of the raw data from CORS station
Download the raw data of active CORS from UNAVCO
Determination of co-ordinates of each station in
different days
Ionospheric
delay correction
Precise
ephemeris
Is horizontal
deviation <5cm and
vertical deviation <
10 cm compared to
ITRF Coordinates of
2016?
ITRF Coordinate
of LHAZ
Identification of active CORS from April 25, 2015 to
May 12, 2015 and January 1, 2017 to January 4, 2017
Literature Review
Processing with new baseline
METHODOLOGY
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Department of Geomatics Engineering9/18/2019
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Computation of shift in Easting, Northing and Vertical
height in each station
Use IDW method for interpolation
Result
Preparation of deformation model
Validated Coordinates with ITRF Coordinate of 2016
Comparison of shift with Shift obtained from
(Nevada Geodetic Laboratory, 2019)
Validation of the model by comparing
data obtained from Survey
Department
Interpolation from IDW
creates the surface passing
through the sample points.
Visualization through Web
map
METHODOLOGY (Continue…)
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Department of Geomatics Engineering
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IDENTIFICATION OF CORS
o Active CORS identified From April 18, 2015 to May 18,
2015 and first four days of 2017.
DOWNLOADING THE RAW DATA
o UNAVCO website
o Download the data in Hatanaka format:
>>> wget –i [Textfile name]
o Convert to appropriate RINEX format using crx2rnx
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POST PROCESSING
• Satlab Geobitz Solution
• LHAZ as base station
• Co-ordinate of base
station was taken from
ITRF website
Title Value/Model
Cut-off angle 15˚
Tropospheric model Saastamoinen
Frequency Auto
Navigation SP3
Systems GPS and GLONASS
Interval 30 seconds
Export Format CSV
Table: Specification table.
Figure: Direction of baseline in Satlab Geobitz Solutions.
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Department of Geomatics Engineering
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DETERMINATION OF COORDINATES OF
EACH STATION IN DIFFERENT DAYS
o Day wise solutions of each station were determined
o Management of coordinates in MS Excel.
VALIDATION OF PROCESSED COORDINATES
o Processed coordinates were compared to ITRF coordinates of
2016.
o Criteria:
• Horizontal deviation should be less than 5cm
• Vertical deviation should be less than 10 cm
o Processing with new baseline if criteria not fulfilled.
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SHIFT COMPUTATION
Equation: Calculation of shift.
𝐹𝑖𝑟𝑠𝑡 𝑆ℎ𝑖𝑓𝑡 =
𝑗=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐴𝑝𝑟25 ,2015
𝑀𝑎𝑦 11,2015
𝐸𝑗
17
−
𝑖=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐴𝑝𝑟𝑖𝑙 18,2015
𝐴𝑝𝑟𝑖𝑙 24 ,2015
𝐸𝑖
7
𝑆𝑒𝑐𝑜𝑛𝑑 𝑠ℎ𝑖𝑓𝑡 =
𝑘=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝑀𝑎𝑦 12 ,2015
𝑀𝑎𝑦 18 ,2015
𝐸 𝑘
7
−
𝑗=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐴𝑝𝑟𝑖𝑙 25 ,2015
𝑀𝑎𝑦 11,2015
𝐸𝑗
17
𝐹𝑖𝑛𝑎𝑙 𝑠ℎ𝑖𝑓𝑡 =
𝑘=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝑀𝑎𝑦 12 ,2015
𝑀𝑎𝑦 18 ,2015
𝐸 𝑘
7
−
𝑖=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐴𝑝𝑟𝑖𝑙 18,2015
𝐴𝑝𝑟𝑖𝑙 24 ,2015
𝐸𝑖
7
𝑅𝑒𝑐𝑒𝑛𝑡 𝑆ℎ𝑖𝑓𝑡 =
𝑙=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐽𝑎𝑛𝑢𝑎𝑟𝑦 1 ,2017
𝐽𝑎𝑛𝑢𝑎𝑟𝑦 4 ,2017
𝐸𝑙
4
−
𝑖=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐴𝑝𝑟𝑖𝑙 18 ,2015
𝐴𝑝𝑟𝑖𝑙 24 ,2015
𝐸𝑖
7
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COMPARISION WITH TIME SERIES PLOT
o The computed shift was compared with the time series plot by Nevada
Geodetic Laboratory.
Figure: Time Series Graph of BESI
Source: (Nevada Geodetic Laboratory, 2019)
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PREPARATION OF DEFORMATION MODEL
o Interpolation using ArcGIS tool to prepare deformation model
o Map layout in ArcGIS
INTERPOLATION TECHNIQUE
o Inverse Distance Weighting
o Follows Tobler’s law; According to Waldo Tobler (GISGeography, 2018)
“Everything is related to everything else, but near things are more
related than distant things.”
o Deterministic method
o Mathematically,
𝑧0 = 𝑖=1
𝑛
𝑤 𝑖 𝑧 𝑖
𝑖=1
𝑛
𝑤 𝑖
(Vineeth, Teja, & Raghuveer, 2019)
Where, 𝑧0 is the value of estimation point
𝑧𝑖 is the value of neighboring point
𝑤𝑖is the weighting factor and 𝑤𝑖= 1/(distance from neighbor)p
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VALIDATION OF MODEL
o Validated the deformation model due to Gorkha earthquake of
April 25, 2015.
o Comparing with the control point stations provided by Survey
Department.
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RESULTS
Table: Day wise coordinates of CHLM station from April 18, 2015 to May 18, 2015
Date Easting (m) Northing (m) Height (m)
May 04 334541.397 3121308.272 3212.408
May 05 334541.362 3121308.337 3212.489
May 06 334541.376 3121308.396 3212.562
May 07 334541.418 3121308.324 3212.569
May 08 334541.415 3121308.321 3212.568
May 09 334541.371 3121308.296 3212.522
May 10 334541.354 3121308.276 3212.454
May 11 334541.394 3121308.263 3212.411
May 12 334541.341 3121308.293 3212.463
May 13 334541.346 3121308.280 3212.497
May 14 334541.394 3121308.208 3212.520
May 15 334541.395 3121308.245 3212.491
May 16 334541.392 3121308.222 3212.466
May 17 334541.407 3121308.262 3212.470
May 18 334541.329 3121308.265 3212.521
Date Easting (m) Northing (m) Height (m)
April 18 334541.574 3121309.696 3213.004
April 19 334541.588 3121309.659 3212.935
April 20 334541.589 3121309.662 3212.979
April 21 334541.596 3121309.699 3213.097
April 22 334541.596 3121309.690 3213.111
April 23 334541.583 3121309.678 3213.013
April 24 334541.546 3121309.695 3213.028
April 25 334541.375 3121308.361 3212.549
April 26 334541.376 3121308.316 3212.460
April 27 334541.366 3121308.263 3212.502
April 28 334541.352 3121308.312 3212.500
April 29 334541.358 3121308.319 3212.410
April 30 334541.353 3121308.236 3212.402
May 01 334541.354 3121308.293 3212.442
May 02 334541.368 3121308.293 3212.457
May 03 334541.361 3121308.290 3212.476
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RESULTS
Stations 1st shift (Due to
earthquake of April 25,
2015 ) (m)
2nd shift (Due to aftershock
of May 12, 2015) (m)
Final shift (Due earthquake
and aftershock) (m)
Total shift till 2017 (m)
dE dN dH dE dN dH dE dN dH dE dN dH
AIRP NDA NDA NDA -0.006 0.001 0.025 NDA NDA NDA NDA NDA NDA
BESI 0.011 -0.016 -0.003 0.002 -0.002 0.012 0.013 -0.018 0.009 0.049 -0.058 0.017
BNDP NDA NDA NDA -0.003 0.008 -0.053 NDA NDA NDA NDA NDA NDA
CHLM -0.208 -1.379 -0.543 -0.001 -0.050 0.009 -0.210 -1.429 -0.534 -0.189 -1.432 -0.461
CHWN 0.021 -0.021 -0.014 0.000 0.011 -0.010 -0.020 -0.010 -0.024 0.048 0.017 -0.017
DNSG -0.006 -0.002 0.027 0.007 0.001 -0.006 0.001 -0.001 0.021 -0.002 -0.010 0.045
GHER 0.034 -0.053 0.023 -0.003 -0.004 0.003 0.031 -0.057 0.026 0.033 -0.090 0.034
JMSM 0.003 0.012 0.008 0.001 0.000 0.002 0.005 0.013 0.010 -0.008 -0.006 0.016
KIRT -0.226 -1.263 0.640 NDA NDA NDA NDA NDA NDA -0.191 -1.176 0.494
KKN4 -0.415 -1.832 1.373 -0.001 0.012 -0.001 -0.416 -1.821 1.371 -0.393 -1.763 1.447
NAST -0.329 -1.287 0.651 -0.012 -0.018 0.036 -0.341 -1.305 0.687 -0.284 -1.240 0.523
RMTE -0.009 0.001 -0.003 0.031 -0.012 0.015 0.022 -0.011 0.012 NDA NDA NDA
SIM4 NDA NDA NDA 0.007 0.003 0.001 NDA NDA NDA NDA NDA NDA
SNDL 0.018 -0.235 0.098 -0.007 0.003 -0.016 0.011 -0.232 0.083 0.064 -0.159 0.051
SYBC 0.011 0.006 0.014 -0.021 -0.050 -0.009 -0.011 -0.044 0.005 -0.059 -0.028 0.015
Table: Shifts of every stations of Gorkha earthquake, aftershock, final shift and total shift till 2017
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RESULTS
Figure: Shift in Northing and easting Of KKN4 located in Kakani, Nepal
from April 18,2015 to May 18,2015
-2.00
-1.90
-1.80
-1.70
-1.60
-1.50
-1.40
-1.30
-1.20
-1.10
-1.00
-0.90
-0.80
-0.70
-0.60
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
April_18
April_19
April_20
April_22
April_23
April_24
April_25
April_26
April_27
April_28
April_29
April_30
May_01
May_02
May_03
May_04
May_05
May_06
May_07
May_08
May_09
May_10
May_11
May_12
May_13
May_14
May_15
May_16
May_17
May_18
Shift(m)
Date (2015 A.D.)
Shift in Easting and Northing April 18 to May 18
(KKN4)
dE dN
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RESULTS
Figure: Graph of Change in Height from April 18 to May 18 of all Stations
-0.800
-0.600
-0.400
-0.200
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600 April_18
April_19
April_20
April_21
April_22
April_23
April_24
April_25
April_26
April_27
April_28
April_29
April_30
May_01s
May_02
May_03
May_04
May_05
May_06
May_07
May_08
May_09
May_10
May_11
May_12
May_13
May_14
May_15
May_16
May_17
May_18
Shift(m)
Date (2015 A.D.)
Change in Height from April 18 to May 18 in all stations
BESI
CHLM
CHWN
DNSG
GHER
JMSM
KIRT
KKN4
NAST
RMTE
SNDL
SYBC
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RESULTS
Figure: Horizontal deformation due to earthquake of April 25, 2015 with the arrows showing deformation
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RESULTS
Figure: Vertical deformation due to earthquake of April 25, 2015
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RESULTS
Figure: Horizontal deformation due to earthquake of May 12, 2015 with the arrows showing deformation
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RESULTS
Figure: Vertical deformation due to earthquake of May 12, 2015
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RESULTS
Figure: Horizontal deformation on CORS due to earthquake of April 25, 2015 and May 12, 2015 with the arrows showing direction of movement of CORS with magnitude
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RESULTS
Figure: Horizontal deformation due to earthquake of April 25, 2015 May 12, 2015 with the arrows showing deformation
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RESULTS
Figure: Vertical deformation due to earthquake of April 25, 2015 and May 12, 2015
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RESULTS
Figure: Horizontal deformation after the successive earthquakes to January, 2017 with the arrows showing deformation
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RESULTS
Figure: Vertical deformation after the successive earthquakes to January, 2017
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VALIDATION OF PROCESSED COORDINATES
o Processed coordinates compared to ITRF coordinates of
2016
Name of Stations Deviations (m)
del E del N del H
BESI -0.013 0.007 -0.032
CHLM -0.023 0.014 -0.049
DNSG -0.032 0.000 -0.016
JMSM 0.033 0.010 -0.080
KKN4 -0.041 0.006 0.140
NAST 0.019 0.034 0.042
SNDL 0.002 -0.020 -0.062
SYBC -0.030 0.030 -0.042
Table: Comparison of processed coordinates with ITRF 2016 coordinates
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COMPARISION WITH TIME SERIES PLOT
o Time series plot by Nevada Geodetic Laboratory(Nevada Geodetic
Laboratory, 2019).
Stations Deviations (mm)
Easting Northing Height
BESI 8 2 -1
CHLM 31 -29 66
CHWN 0 0 NDA
DNSG -4 -2 1
GHER 1 -17 76
JMSM 0 23 NDA
KKN4 4 -21 71
NAST -1 -5 37
RMTE 2 -1 0
SNDL -9 -12 NDA
SYBC 4 -4 NDA
Table: Comparison of computed shift with Nevada Geodetic Laboratory
*The comparison is approximate because the graph provided by Nevada Geodetic Laboratory was without the data in
table and we had to do eye estimation.
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VALIDATION OF INTERPOLATED RESULT
o Comparing with the control point stations provided by Survey
Department.
Station Id Standard value of Shift (m) Values from the Deformation
Map due to Gorkha Earthquake
(m)
Deviation (m)
Horizontal Height Horizontal Height ∆Horizontal ∆Height
Fulchoki 0.923 0.631 1.284 0.567 -0.361 0.064
Swoyambhu 1.642 0.983 1.347 0.712 0.295 0.271
Nagarkot 1.825 1.158 1.278 0.670 0.547 0.488
Kumari 1.719 1.093 1.505 0.910 0.214 0.183
Lakhedada 0.994 0.770 1.323 0.659 -0.329 0.111
Table: Validation of Deformation Model
Source: (Survey Department, 2015)
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RESULTS
Figure: Deformation model due to earthquakes shown in the web
o Visualization in the form of web
o Demo :
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CONCLUSION AND RECOMMENDATION
o Unequal shift in affected regions.
o Central part of the study area has shifted in the south east
direction.
o Deformation can be used to assess the accuracy of control points
used for various purposes.
o Use of fixed control points should be discouraged.
o Number of CORS should be more and should have proper
geographical distribution.
o Data should be continuous.
o The network adjustment can be done by using shortest possible
unaffected baseline.
o Use of other interpolation technique might increase the accuracy
of model.
o 3D plots would provide better visualization.
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REFERENCES
o GISGeography. (2018, May 31). Tobler first law of geography.
Retrieved September 01, 2019, from GISGeography:
https://gisgeography.com/tobler-first-law-of-geography/
o International Terrestrial Reference Frame. (2016). Solution Extraction.
Retrieved July 05, 2019, from ITRF:
http://itrf.ensg.ign.fr/site_info_and_select/solutions_extraction.php
o Jahic, E. (2016). GNSS Calendar. Retrieved July 05, 2019, from GNSS
Calendar: http://gnsscalendar.com/
o Nevada Geodetic Laboratory. (2019, July 07). Retrieved August 14,
2019, from http://geodesy.unr.edu/tsplots/IGS08/TimeSeries/
o Rafferty, J. P. (2019). Nepal earthquake of 2015. Retrieved from
Britannica: https://www.britannica.com/place/Nepal
o UNAVCO. (2019). Data Archive Interface. Retrieved January 29, 2019,
from UNAVCO: https://www.unavco.org/data/gps-gnss/data-access-
methods/dai2/app/dai2.html#grouping=nepal
o Vineeth, P., Teja, K. S., & Raghuveer, D. (2019). Inverse Distance
Weighting. Retrieved from slideshare:
https://www.slideshare.net/penchalavineeth/inverse-distance-weighting
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THANK
YOU!
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ANNEXES
Station name Interval Location Lat (˚) Long(˚) Height (m) Started at last operating (as
per 1st
february,2019)
Grouping
AIRP 15.0 sec Tribhuvan
International
Airport
27.6972 85.3579 1289 2015 May 11 06:04 2015 Jul 24 23:59 Nepal
BELT 15.0 sec Belatari 27.457 83.826 54.32 2008 Jul 06 06:04 2017 Feb 03 23:59 Nepal
BESI 15.0 sec Besisahar 28.2286 84.3797 738.0416 2008 Jun 28 11:56 2019 Jan 15 05:36 Nepal
BNDP 15.0 sec Bandipur_NPL2012 27.9495 84.3951 775.2039 2015 May 02 10:25 2016 Jul 16 23:59 NEGAR Nepal
CHLM 15.0 sec Chilime 28.2072 85.3141 3212.539 2004 Mar 31 08:58 2019 Jan 30 23:59 NEGAR Nepal
CHWN 15.0 sec Chitwan 27.6682 84.3853 133.4 2011 Mar 28 08:34 2019 Jan 30 23:59 NEGAR Nepal
DMAU 15.0 sec Damauli 27.973 84.265 299.91 2008 Jul 05 08:58 2016 May 22 10:17 Nepal
DNSG 15.0 sec Dansing 28.3451 83.7635 2427.346 2012 Apr 29 10:30 2019 Jan 29 23:59 NEGAR Nepal
GHER 15.0 sec Ghermu 28.375 84.41 1530.42 2008 Jul 03 09:51 2017 Feb 06 23:59 Nepal
JMSM 15.0 sec Jomsom 28.8053 83.7433 3438.296 2004 May 02 11:02 2019 Jan 24 23:59 NEGAR Nepal
KIRT 15.0 sec Kirtipur 27.682 85.288 1277.32 2008 Jun 19 08:03 2017 Feb 07 23:59 Nepal
KKN4 15.0 sec Kakani 4 27.8007 85.2788 1898.468 2004 Mar 22 10:00 2017 Sep 26 23:59 NEGAR Nepal
NAST 15.0 sec NAST_SciTec_2013 27.6567 85.3277 1278.429 2014 Jan 18 00:00 2019 Jan 30 23:59 NEGAR Nepal
RMTE 15.0 sec Ramite 26.991 86.5971 2074 2008 Sep 23 13:59 2016 Mar 10 23:59 NEGAR Nepal
SIM4 15.0 sec Simara 4 27.1656 84.9852 71.8997 2004 Mar 26 00:00 2016 May 20 23:59 NEGAR Nepal
SNDL 15.0 sec Sindhuli 27.3848 85.7989 2002.731 2011 Apr 05 12:09 2019 Jan 30 23:59 NEGAR Nepal
SYBC 15.0 sec Syangboche 27.8142 86.7125 3794.245 2008 Oct 04 04:34 2019 Jan 26 23:59 NEGAR Nepal
Table: List of CORS with Details extracted on 2nd February 2019
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ANNEXES
Source: (Nevada Geodetic Laboratory, 2019)
Figure: Time Series Graph of CHLMFigure: Time Series Graph of BESI Figure: Time Series Graph of CHWN Figure: Time Series Graph of JMSM
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ANNEXES
Source: (Nevada Geodetic Laboratory, 2019)
Figure: Time Series Graph of NASTFigure: Time Series Graph of KKN4 Figure: Time Series Graph of SYBC Figure: Time Series Graph of SNDL
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ANNEXES
1. Reference:
Marker name: LHAZ
Marker code: 21613M002
WGS84 X (m): -106941.9243
WGS84 Y (m): 5549269.8010
WGS84 Z (m): 3139215.1485
WGS84 latitude: 029:39:246. 0036N
WGS84 longitude: 091:06:14.50944E
WGS84 height :( m): 3624.6076
Receiver type: TPS E_GGD
Receiver version: 3.4 DEC, 12, 2009 P2
Receiver S/N: AE7PEWVFA4G
Antenna type: ASH701941.B SNOW
Antenna S/N
Antenna height :(m) 0.1330
Measured to: Anttena Bottom
2. Rover:
Marker name: CHLM
Marker code:
WGS84 X (m): 459749.0644
WGS84 Y (m): 5608922.2740
WGS84 Z (m): 2998281.8881
WGS84 latitude: 028:12:26.03496N
WGS84 longitude: 085:18:50.71174E
WGS84 height :( m): 3213.0041
Receiver type: TRIMBLE NETR8
Receiver version: 4.70
Receiver S/N: 5011K66180
Antenna type: ASH701945E_M SCIT
Antenna S/N
Antenna height :( m) 0.0083
Measured to: Anttena Bottom
3. Processing controls:
Start time: 4/18/2015 5:45:30 AM
Stop time: 4/19/2015 5:44:30 AM
Required solution type: Auto
Elevation mask [deg]: 15
Tropospheric delay model: Saastamoinen
Orbit type: Precise
Single frequency fixed baseline mask: [m]:30000
*This is a report generated by the Satlab Geobitz Solution software during the post processing of raw data for the baseline LHAZ to CHLM
ITRF coordinate of 2016 Coordinates used for validation
9/18/2019
41
Name Longitude ( ˚ ) Latitude ( ˚ ) Height (m)
BESI 84.37967 28.22861 738.0416
CHLM 85.31408 28.20722 3212.539
DNSG 83.76346 28.34509 2427.346
JMSM 83.7433 28.80528 3438.296
KKN4 85.2788 27.80071 1898.468
NAST 85.32773 27.65668 1278.429
SNDL 85.79886 27.38483 2002.731
SYBC 86.71246 27.81423 3794.245

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Presentation slide on Project entitled "Preparation of Deformation Model of Central Nepal Due to Gorkha Earthquake 2015 And the Aftershock"

  • 1. Kathmandu University Department of Geomatics Engineering Presenter A PRESENTATION ON PREPARATION OF DEFORMATION MODEL OF CENTRAL NEPAL DUE TO GORKHA EARTHQUAKE 2015 AND THE AFTERSHOCK Ashmita Dhakal | Rohit Gautam | Aakash Thapa | Prashant Thapaliya
  • 2. Kathmandu University Department of Geomatics Engineering 2 9/18/2019 INTRODUCTION o On April 25, 2015, Gorkha earthquake of 7.8 moment magnitude occurred causing death of around 9,000 people. o Thousands were injured and more than 6 lakhs structures in Kathmandu were damaged or destroyed. o On May 12,2015, aftershock of 7.3 Mw struck in Dolakha killing more than 100 people. o Compressional pressure between Eurasian tectonic plate and Indian section of Indo-Australian Plate; subducts the Eurasian Plate (Rafferty, 2019). o Deformation of surface o CORS
  • 3. Kathmandu University Department of Geomatics Engineering 3 9/18/2019 PROBLEM STATEMENT o No revision and update of control points in Nepal. o No significant steps taken by authority to calculate deformation. o Existing maps prepared by Survey Department long time ago need to be updated.
  • 4. Kathmandu University Department of Geomatics Engineering 4 9/18/2019 OBJECTIVES Primary Objective Prepare deformation model of central Nepal due to Gorkha Earthquake 2015 and the aftershock. Secondary Objectives To determine northing, easting and vertical shift of each station. To interpolate the deformation on ground between the stations. To visualize result in web
  • 5. 9/18/2019 5 Bounding box: • 2985496.754 m to 3190768.567 m in northing • 182112.662 m to 471679.824 m in easting STUDY AREA Figure: Map of Nepal showing the study area Area- 42000 sq. km
  • 6. Kathmandu University Department of Geomatics Engineering 6 9/18/2019 DATA SOURCES UNAVCO (UNAVCO, 2019) To download data of CORS ITRF (International Terrestrial Reference Frame, 2016) To obtain the coordinates of base station for post processing GNSS Calendar (Jahic, 2016) To download SP3 files NEVADA Geodetic Laboratory (Nevada Geodetic Laboratory, 2019) To compare the shift computed with the shift available in the website
  • 7. Kathmandu University Department of Geomatics Engineering 7 9/18/2019 SOFTWARE USED Satlab Geobitz Solutions To post-processing data in RINEX to produce more accurate result ArcGIS To interpolate, visualization and map layout MS Office Packages Microsoft Excel for data manipulation, analysis, management and calculation and MS Word to prepare the report Visual Studio Code To write codes for web app
  • 8. Kathmandu University Department of Geomatics Engineering9/18/2019 8 No Yes Validated Coordinates with ITRF Coordinate of 2016 Post Processing of the raw data from CORS station Download the raw data of active CORS from UNAVCO Determination of co-ordinates of each station in different days Ionospheric delay correction Precise ephemeris Is horizontal deviation <5cm and vertical deviation < 10 cm compared to ITRF Coordinates of 2016? ITRF Coordinate of LHAZ Identification of active CORS from April 25, 2015 to May 12, 2015 and January 1, 2017 to January 4, 2017 Literature Review Processing with new baseline METHODOLOGY
  • 9. Kathmandu University Department of Geomatics Engineering9/18/2019 9 Computation of shift in Easting, Northing and Vertical height in each station Use IDW method for interpolation Result Preparation of deformation model Validated Coordinates with ITRF Coordinate of 2016 Comparison of shift with Shift obtained from (Nevada Geodetic Laboratory, 2019) Validation of the model by comparing data obtained from Survey Department Interpolation from IDW creates the surface passing through the sample points. Visualization through Web map METHODOLOGY (Continue…)
  • 10. Kathmandu University Department of Geomatics Engineering 10 9/18/2019 IDENTIFICATION OF CORS o Active CORS identified From April 18, 2015 to May 18, 2015 and first four days of 2017. DOWNLOADING THE RAW DATA o UNAVCO website o Download the data in Hatanaka format: >>> wget –i [Textfile name] o Convert to appropriate RINEX format using crx2rnx
  • 11. Kathmandu University Department of Geomatics Engineering 11 9/18/2019 POST PROCESSING • Satlab Geobitz Solution • LHAZ as base station • Co-ordinate of base station was taken from ITRF website Title Value/Model Cut-off angle 15˚ Tropospheric model Saastamoinen Frequency Auto Navigation SP3 Systems GPS and GLONASS Interval 30 seconds Export Format CSV Table: Specification table. Figure: Direction of baseline in Satlab Geobitz Solutions.
  • 12. Kathmandu University Department of Geomatics Engineering 12 9/18/2019 DETERMINATION OF COORDINATES OF EACH STATION IN DIFFERENT DAYS o Day wise solutions of each station were determined o Management of coordinates in MS Excel. VALIDATION OF PROCESSED COORDINATES o Processed coordinates were compared to ITRF coordinates of 2016. o Criteria: • Horizontal deviation should be less than 5cm • Vertical deviation should be less than 10 cm o Processing with new baseline if criteria not fulfilled.
  • 13. Kathmandu University Department of Geomatics Engineering 13 9/18/2019 SHIFT COMPUTATION Equation: Calculation of shift. 𝐹𝑖𝑟𝑠𝑡 𝑆ℎ𝑖𝑓𝑡 = 𝑗=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐴𝑝𝑟25 ,2015 𝑀𝑎𝑦 11,2015 𝐸𝑗 17 − 𝑖=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐴𝑝𝑟𝑖𝑙 18,2015 𝐴𝑝𝑟𝑖𝑙 24 ,2015 𝐸𝑖 7 𝑆𝑒𝑐𝑜𝑛𝑑 𝑠ℎ𝑖𝑓𝑡 = 𝑘=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝑀𝑎𝑦 12 ,2015 𝑀𝑎𝑦 18 ,2015 𝐸 𝑘 7 − 𝑗=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐴𝑝𝑟𝑖𝑙 25 ,2015 𝑀𝑎𝑦 11,2015 𝐸𝑗 17 𝐹𝑖𝑛𝑎𝑙 𝑠ℎ𝑖𝑓𝑡 = 𝑘=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝑀𝑎𝑦 12 ,2015 𝑀𝑎𝑦 18 ,2015 𝐸 𝑘 7 − 𝑖=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐴𝑝𝑟𝑖𝑙 18,2015 𝐴𝑝𝑟𝑖𝑙 24 ,2015 𝐸𝑖 7 𝑅𝑒𝑐𝑒𝑛𝑡 𝑆ℎ𝑖𝑓𝑡 = 𝑙=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐽𝑎𝑛𝑢𝑎𝑟𝑦 1 ,2017 𝐽𝑎𝑛𝑢𝑎𝑟𝑦 4 ,2017 𝐸𝑙 4 − 𝑖=𝑒𝑎𝑠𝑡𝑖𝑛𝑔 𝑜𝑓 𝐴𝑝𝑟𝑖𝑙 18 ,2015 𝐴𝑝𝑟𝑖𝑙 24 ,2015 𝐸𝑖 7
  • 14. Kathmandu University Department of Geomatics Engineering 14 9/18/2019 COMPARISION WITH TIME SERIES PLOT o The computed shift was compared with the time series plot by Nevada Geodetic Laboratory. Figure: Time Series Graph of BESI Source: (Nevada Geodetic Laboratory, 2019)
  • 15. Kathmandu University Department of Geomatics Engineering 15 9/18/2019 PREPARATION OF DEFORMATION MODEL o Interpolation using ArcGIS tool to prepare deformation model o Map layout in ArcGIS INTERPOLATION TECHNIQUE o Inverse Distance Weighting o Follows Tobler’s law; According to Waldo Tobler (GISGeography, 2018) “Everything is related to everything else, but near things are more related than distant things.” o Deterministic method o Mathematically, 𝑧0 = 𝑖=1 𝑛 𝑤 𝑖 𝑧 𝑖 𝑖=1 𝑛 𝑤 𝑖 (Vineeth, Teja, & Raghuveer, 2019) Where, 𝑧0 is the value of estimation point 𝑧𝑖 is the value of neighboring point 𝑤𝑖is the weighting factor and 𝑤𝑖= 1/(distance from neighbor)p
  • 16. Kathmandu University Department of Geomatics Engineering 16 9/18/2019 VALIDATION OF MODEL o Validated the deformation model due to Gorkha earthquake of April 25, 2015. o Comparing with the control point stations provided by Survey Department.
  • 17. Kathmandu University Department of Geomatics Engineering 17 9/18/2019 RESULTS Table: Day wise coordinates of CHLM station from April 18, 2015 to May 18, 2015 Date Easting (m) Northing (m) Height (m) May 04 334541.397 3121308.272 3212.408 May 05 334541.362 3121308.337 3212.489 May 06 334541.376 3121308.396 3212.562 May 07 334541.418 3121308.324 3212.569 May 08 334541.415 3121308.321 3212.568 May 09 334541.371 3121308.296 3212.522 May 10 334541.354 3121308.276 3212.454 May 11 334541.394 3121308.263 3212.411 May 12 334541.341 3121308.293 3212.463 May 13 334541.346 3121308.280 3212.497 May 14 334541.394 3121308.208 3212.520 May 15 334541.395 3121308.245 3212.491 May 16 334541.392 3121308.222 3212.466 May 17 334541.407 3121308.262 3212.470 May 18 334541.329 3121308.265 3212.521 Date Easting (m) Northing (m) Height (m) April 18 334541.574 3121309.696 3213.004 April 19 334541.588 3121309.659 3212.935 April 20 334541.589 3121309.662 3212.979 April 21 334541.596 3121309.699 3213.097 April 22 334541.596 3121309.690 3213.111 April 23 334541.583 3121309.678 3213.013 April 24 334541.546 3121309.695 3213.028 April 25 334541.375 3121308.361 3212.549 April 26 334541.376 3121308.316 3212.460 April 27 334541.366 3121308.263 3212.502 April 28 334541.352 3121308.312 3212.500 April 29 334541.358 3121308.319 3212.410 April 30 334541.353 3121308.236 3212.402 May 01 334541.354 3121308.293 3212.442 May 02 334541.368 3121308.293 3212.457 May 03 334541.361 3121308.290 3212.476
  • 18. Kathmandu University Department of Geomatics Engineering 18 9/18/2019 RESULTS Stations 1st shift (Due to earthquake of April 25, 2015 ) (m) 2nd shift (Due to aftershock of May 12, 2015) (m) Final shift (Due earthquake and aftershock) (m) Total shift till 2017 (m) dE dN dH dE dN dH dE dN dH dE dN dH AIRP NDA NDA NDA -0.006 0.001 0.025 NDA NDA NDA NDA NDA NDA BESI 0.011 -0.016 -0.003 0.002 -0.002 0.012 0.013 -0.018 0.009 0.049 -0.058 0.017 BNDP NDA NDA NDA -0.003 0.008 -0.053 NDA NDA NDA NDA NDA NDA CHLM -0.208 -1.379 -0.543 -0.001 -0.050 0.009 -0.210 -1.429 -0.534 -0.189 -1.432 -0.461 CHWN 0.021 -0.021 -0.014 0.000 0.011 -0.010 -0.020 -0.010 -0.024 0.048 0.017 -0.017 DNSG -0.006 -0.002 0.027 0.007 0.001 -0.006 0.001 -0.001 0.021 -0.002 -0.010 0.045 GHER 0.034 -0.053 0.023 -0.003 -0.004 0.003 0.031 -0.057 0.026 0.033 -0.090 0.034 JMSM 0.003 0.012 0.008 0.001 0.000 0.002 0.005 0.013 0.010 -0.008 -0.006 0.016 KIRT -0.226 -1.263 0.640 NDA NDA NDA NDA NDA NDA -0.191 -1.176 0.494 KKN4 -0.415 -1.832 1.373 -0.001 0.012 -0.001 -0.416 -1.821 1.371 -0.393 -1.763 1.447 NAST -0.329 -1.287 0.651 -0.012 -0.018 0.036 -0.341 -1.305 0.687 -0.284 -1.240 0.523 RMTE -0.009 0.001 -0.003 0.031 -0.012 0.015 0.022 -0.011 0.012 NDA NDA NDA SIM4 NDA NDA NDA 0.007 0.003 0.001 NDA NDA NDA NDA NDA NDA SNDL 0.018 -0.235 0.098 -0.007 0.003 -0.016 0.011 -0.232 0.083 0.064 -0.159 0.051 SYBC 0.011 0.006 0.014 -0.021 -0.050 -0.009 -0.011 -0.044 0.005 -0.059 -0.028 0.015 Table: Shifts of every stations of Gorkha earthquake, aftershock, final shift and total shift till 2017
  • 19. Kathmandu University Department of Geomatics Engineering 19 9/18/2019 RESULTS Figure: Shift in Northing and easting Of KKN4 located in Kakani, Nepal from April 18,2015 to May 18,2015 -2.00 -1.90 -1.80 -1.70 -1.60 -1.50 -1.40 -1.30 -1.20 -1.10 -1.00 -0.90 -0.80 -0.70 -0.60 -0.50 -0.40 -0.30 -0.20 -0.10 0.00 0.10 April_18 April_19 April_20 April_22 April_23 April_24 April_25 April_26 April_27 April_28 April_29 April_30 May_01 May_02 May_03 May_04 May_05 May_06 May_07 May_08 May_09 May_10 May_11 May_12 May_13 May_14 May_15 May_16 May_17 May_18 Shift(m) Date (2015 A.D.) Shift in Easting and Northing April 18 to May 18 (KKN4) dE dN
  • 20. Kathmandu University Department of Geomatics Engineering 20 9/18/2019 RESULTS Figure: Graph of Change in Height from April 18 to May 18 of all Stations -0.800 -0.600 -0.400 -0.200 0.000 0.200 0.400 0.600 0.800 1.000 1.200 1.400 1.600 April_18 April_19 April_20 April_21 April_22 April_23 April_24 April_25 April_26 April_27 April_28 April_29 April_30 May_01s May_02 May_03 May_04 May_05 May_06 May_07 May_08 May_09 May_10 May_11 May_12 May_13 May_14 May_15 May_16 May_17 May_18 Shift(m) Date (2015 A.D.) Change in Height from April 18 to May 18 in all stations BESI CHLM CHWN DNSG GHER JMSM KIRT KKN4 NAST RMTE SNDL SYBC
  • 21. Kathmandu University Department of Geomatics Engineering 21 9/18/2019 RESULTS Figure: Horizontal deformation due to earthquake of April 25, 2015 with the arrows showing deformation
  • 22. Kathmandu University Department of Geomatics Engineering 22 9/18/2019 RESULTS Figure: Vertical deformation due to earthquake of April 25, 2015
  • 23. Kathmandu University Department of Geomatics Engineering 23 9/18/2019 RESULTS Figure: Horizontal deformation due to earthquake of May 12, 2015 with the arrows showing deformation
  • 24. Kathmandu University Department of Geomatics Engineering 24 9/18/2019 RESULTS Figure: Vertical deformation due to earthquake of May 12, 2015
  • 25. Kathmandu University Department of Geomatics Engineering 25 9/18/2019 RESULTS Figure: Horizontal deformation on CORS due to earthquake of April 25, 2015 and May 12, 2015 with the arrows showing direction of movement of CORS with magnitude
  • 26. Kathmandu University Department of Geomatics Engineering 26 9/18/2019 RESULTS Figure: Horizontal deformation due to earthquake of April 25, 2015 May 12, 2015 with the arrows showing deformation
  • 27. Kathmandu University Department of Geomatics Engineering 27 9/18/2019 RESULTS Figure: Vertical deformation due to earthquake of April 25, 2015 and May 12, 2015
  • 28. Kathmandu University Department of Geomatics Engineering 28 9/18/2019 RESULTS Figure: Horizontal deformation after the successive earthquakes to January, 2017 with the arrows showing deformation
  • 29. Kathmandu University Department of Geomatics Engineering 29 9/18/2019 RESULTS Figure: Vertical deformation after the successive earthquakes to January, 2017
  • 30. Kathmandu University Department of Geomatics Engineering 30 9/18/2019 VALIDATION OF PROCESSED COORDINATES o Processed coordinates compared to ITRF coordinates of 2016 Name of Stations Deviations (m) del E del N del H BESI -0.013 0.007 -0.032 CHLM -0.023 0.014 -0.049 DNSG -0.032 0.000 -0.016 JMSM 0.033 0.010 -0.080 KKN4 -0.041 0.006 0.140 NAST 0.019 0.034 0.042 SNDL 0.002 -0.020 -0.062 SYBC -0.030 0.030 -0.042 Table: Comparison of processed coordinates with ITRF 2016 coordinates
  • 31. Kathmandu University Department of Geomatics Engineering 31 9/18/2019 COMPARISION WITH TIME SERIES PLOT o Time series plot by Nevada Geodetic Laboratory(Nevada Geodetic Laboratory, 2019). Stations Deviations (mm) Easting Northing Height BESI 8 2 -1 CHLM 31 -29 66 CHWN 0 0 NDA DNSG -4 -2 1 GHER 1 -17 76 JMSM 0 23 NDA KKN4 4 -21 71 NAST -1 -5 37 RMTE 2 -1 0 SNDL -9 -12 NDA SYBC 4 -4 NDA Table: Comparison of computed shift with Nevada Geodetic Laboratory *The comparison is approximate because the graph provided by Nevada Geodetic Laboratory was without the data in table and we had to do eye estimation.
  • 32. Kathmandu University Department of Geomatics Engineering 32 9/18/2019 VALIDATION OF INTERPOLATED RESULT o Comparing with the control point stations provided by Survey Department. Station Id Standard value of Shift (m) Values from the Deformation Map due to Gorkha Earthquake (m) Deviation (m) Horizontal Height Horizontal Height ∆Horizontal ∆Height Fulchoki 0.923 0.631 1.284 0.567 -0.361 0.064 Swoyambhu 1.642 0.983 1.347 0.712 0.295 0.271 Nagarkot 1.825 1.158 1.278 0.670 0.547 0.488 Kumari 1.719 1.093 1.505 0.910 0.214 0.183 Lakhedada 0.994 0.770 1.323 0.659 -0.329 0.111 Table: Validation of Deformation Model Source: (Survey Department, 2015)
  • 33. Kathmandu University Department of Geomatics Engineering 33 9/18/2019 RESULTS Figure: Deformation model due to earthquakes shown in the web o Visualization in the form of web o Demo :
  • 34. Kathmandu University Department of Geomatics Engineering 34 9/18/2019 CONCLUSION AND RECOMMENDATION o Unequal shift in affected regions. o Central part of the study area has shifted in the south east direction. o Deformation can be used to assess the accuracy of control points used for various purposes. o Use of fixed control points should be discouraged. o Number of CORS should be more and should have proper geographical distribution. o Data should be continuous. o The network adjustment can be done by using shortest possible unaffected baseline. o Use of other interpolation technique might increase the accuracy of model. o 3D plots would provide better visualization.
  • 35. Kathmandu University Department of Geomatics Engineering 35 9/18/2019 REFERENCES o GISGeography. (2018, May 31). Tobler first law of geography. Retrieved September 01, 2019, from GISGeography: https://gisgeography.com/tobler-first-law-of-geography/ o International Terrestrial Reference Frame. (2016). Solution Extraction. Retrieved July 05, 2019, from ITRF: http://itrf.ensg.ign.fr/site_info_and_select/solutions_extraction.php o Jahic, E. (2016). GNSS Calendar. Retrieved July 05, 2019, from GNSS Calendar: http://gnsscalendar.com/ o Nevada Geodetic Laboratory. (2019, July 07). Retrieved August 14, 2019, from http://geodesy.unr.edu/tsplots/IGS08/TimeSeries/ o Rafferty, J. P. (2019). Nepal earthquake of 2015. Retrieved from Britannica: https://www.britannica.com/place/Nepal o UNAVCO. (2019). Data Archive Interface. Retrieved January 29, 2019, from UNAVCO: https://www.unavco.org/data/gps-gnss/data-access- methods/dai2/app/dai2.html#grouping=nepal o Vineeth, P., Teja, K. S., & Raghuveer, D. (2019). Inverse Distance Weighting. Retrieved from slideshare: https://www.slideshare.net/penchalavineeth/inverse-distance-weighting
  • 36. Kathmandu University Department of Geomatics Engineering9/18/2019 36 THANK YOU!
  • 37. Kathmandu University Department of Geomatics Engineering 37 9/18/2019 ANNEXES Station name Interval Location Lat (˚) Long(˚) Height (m) Started at last operating (as per 1st february,2019) Grouping AIRP 15.0 sec Tribhuvan International Airport 27.6972 85.3579 1289 2015 May 11 06:04 2015 Jul 24 23:59 Nepal BELT 15.0 sec Belatari 27.457 83.826 54.32 2008 Jul 06 06:04 2017 Feb 03 23:59 Nepal BESI 15.0 sec Besisahar 28.2286 84.3797 738.0416 2008 Jun 28 11:56 2019 Jan 15 05:36 Nepal BNDP 15.0 sec Bandipur_NPL2012 27.9495 84.3951 775.2039 2015 May 02 10:25 2016 Jul 16 23:59 NEGAR Nepal CHLM 15.0 sec Chilime 28.2072 85.3141 3212.539 2004 Mar 31 08:58 2019 Jan 30 23:59 NEGAR Nepal CHWN 15.0 sec Chitwan 27.6682 84.3853 133.4 2011 Mar 28 08:34 2019 Jan 30 23:59 NEGAR Nepal DMAU 15.0 sec Damauli 27.973 84.265 299.91 2008 Jul 05 08:58 2016 May 22 10:17 Nepal DNSG 15.0 sec Dansing 28.3451 83.7635 2427.346 2012 Apr 29 10:30 2019 Jan 29 23:59 NEGAR Nepal GHER 15.0 sec Ghermu 28.375 84.41 1530.42 2008 Jul 03 09:51 2017 Feb 06 23:59 Nepal JMSM 15.0 sec Jomsom 28.8053 83.7433 3438.296 2004 May 02 11:02 2019 Jan 24 23:59 NEGAR Nepal KIRT 15.0 sec Kirtipur 27.682 85.288 1277.32 2008 Jun 19 08:03 2017 Feb 07 23:59 Nepal KKN4 15.0 sec Kakani 4 27.8007 85.2788 1898.468 2004 Mar 22 10:00 2017 Sep 26 23:59 NEGAR Nepal NAST 15.0 sec NAST_SciTec_2013 27.6567 85.3277 1278.429 2014 Jan 18 00:00 2019 Jan 30 23:59 NEGAR Nepal RMTE 15.0 sec Ramite 26.991 86.5971 2074 2008 Sep 23 13:59 2016 Mar 10 23:59 NEGAR Nepal SIM4 15.0 sec Simara 4 27.1656 84.9852 71.8997 2004 Mar 26 00:00 2016 May 20 23:59 NEGAR Nepal SNDL 15.0 sec Sindhuli 27.3848 85.7989 2002.731 2011 Apr 05 12:09 2019 Jan 30 23:59 NEGAR Nepal SYBC 15.0 sec Syangboche 27.8142 86.7125 3794.245 2008 Oct 04 04:34 2019 Jan 26 23:59 NEGAR Nepal Table: List of CORS with Details extracted on 2nd February 2019
  • 38. Kathmandu University Department of Geomatics Engineering 38 9/18/2019 ANNEXES Source: (Nevada Geodetic Laboratory, 2019) Figure: Time Series Graph of CHLMFigure: Time Series Graph of BESI Figure: Time Series Graph of CHWN Figure: Time Series Graph of JMSM
  • 39. Kathmandu University Department of Geomatics Engineering 39 9/18/2019 ANNEXES Source: (Nevada Geodetic Laboratory, 2019) Figure: Time Series Graph of NASTFigure: Time Series Graph of KKN4 Figure: Time Series Graph of SYBC Figure: Time Series Graph of SNDL
  • 40. Kathmandu University Department of Geomatics Engineering 40 9/18/2019 ANNEXES 1. Reference: Marker name: LHAZ Marker code: 21613M002 WGS84 X (m): -106941.9243 WGS84 Y (m): 5549269.8010 WGS84 Z (m): 3139215.1485 WGS84 latitude: 029:39:246. 0036N WGS84 longitude: 091:06:14.50944E WGS84 height :( m): 3624.6076 Receiver type: TPS E_GGD Receiver version: 3.4 DEC, 12, 2009 P2 Receiver S/N: AE7PEWVFA4G Antenna type: ASH701941.B SNOW Antenna S/N Antenna height :(m) 0.1330 Measured to: Anttena Bottom 2. Rover: Marker name: CHLM Marker code: WGS84 X (m): 459749.0644 WGS84 Y (m): 5608922.2740 WGS84 Z (m): 2998281.8881 WGS84 latitude: 028:12:26.03496N WGS84 longitude: 085:18:50.71174E WGS84 height :( m): 3213.0041 Receiver type: TRIMBLE NETR8 Receiver version: 4.70 Receiver S/N: 5011K66180 Antenna type: ASH701945E_M SCIT Antenna S/N Antenna height :( m) 0.0083 Measured to: Anttena Bottom 3. Processing controls: Start time: 4/18/2015 5:45:30 AM Stop time: 4/19/2015 5:44:30 AM Required solution type: Auto Elevation mask [deg]: 15 Tropospheric delay model: Saastamoinen Orbit type: Precise Single frequency fixed baseline mask: [m]:30000 *This is a report generated by the Satlab Geobitz Solution software during the post processing of raw data for the baseline LHAZ to CHLM
  • 41. ITRF coordinate of 2016 Coordinates used for validation 9/18/2019 41 Name Longitude ( ˚ ) Latitude ( ˚ ) Height (m) BESI 84.37967 28.22861 738.0416 CHLM 85.31408 28.20722 3212.539 DNSG 83.76346 28.34509 2427.346 JMSM 83.7433 28.80528 3438.296 KKN4 85.2788 27.80071 1898.468 NAST 85.32773 27.65668 1278.429 SNDL 85.79886 27.38483 2002.731 SYBC 86.71246 27.81423 3794.245