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Page 1: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Datum Evolution

Page 2: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

A  Horizontal  Datum  is  reference  surface;  a  

datum  realization  is  an  estimate  of  the  location  of  

a  set  of  points  on  the  surface

Page 3: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

A  Vertical  Datum  is  reference  surface;  a  

datum  realization  is  an  estimate  of  the  height  of  a  set  of  points  above  the  

surface

Page 4: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

To  Recent  Present:  Horizontal  and  Vertical  Survey  Benchmarks

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Page 5: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Now: Accurate, anytime, anywhere positioning

Page 6: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Establishing  a  Datum

Horizontal  and  vertical  datums  are  realized  through  large  survey  networks  

1. Define  the  shape  of  the  Earth  (the  ellipsoid)  2. Accurately  measure  the  position  of  a  set  of  

control  points  on  the  ellipsoid    3. Calculate/adjust  the  reference  surface  and  

network,  document  these  so  they  may  be  use  as  a  reference  against  which  all  other  points  will  be  measured

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Page 7: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,
Page 8: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

U.S. Datums through Time

We’ve had several major datums, soon to have another (by 2022)

NAD27, with NGVD29, no geoid

NAD83(86) with NAVD88, geoid 03

NAD83(HARN/HPGN), with NAVD83, geoid 03

NAD83(1996), with NAVD88, geoid 03

NAD83(NSRS2007), with NAVD88, geoid 09

NAD83(2011), with NAVD88, geoid 12B

Page 9: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Why  change  datums/Realizations

• NAD27       based  on  old  observations  and  old  system  • NAD83(86)    based  on  old  observations  and  new  system  • NAD83(92)    based  on  old  and  new  observations,  same  system  • NAD83(96)  based  on  newer  observations,  same  system  • NAD83(NSRS2007)    new  observations,  same  system,  removed  

regional  distortions  and  made  consistent  with  CORS  • NAD83(2011)  based  on  new  observations  and  same  system.    

Kept  consistent  with  CORS  • 2022  will  be  based  on  new  observations  and  new  (Earth  

centered)  system

Page 10: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

North  American  Datum  of  1927,    26,000  measured  points,  Clarke  1866  spheroid,  fixed  starting  point  in  Kansas  -­‐  not  Earth  centered

NAD27 survey network 10

Page 11: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Fixed location in Kansas, Propagated Error from There

Page 12: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Vertical Datum NGVD29 based on physical/optical leveling, tied to several MSL gauges

Page 13: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,
Page 14: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

By  1970s,  more  and  better  measurements,  better  ellipsoid  (GRS80)  hence  new  datum,  NAD  83  (1986)

• Original  realization  completed  in  1986  – Consisted  (almost)  entirely  of  classical  (optical)  

observations  • “High  Precision  Geodetic  Network”  (HPGN)  and  

“High  Accuracy  Reference  Network”  (HARN)  realizations,  GPS  was  sooooo  much  better  – Most  done  in  1990s,  essentially  state-­‐by-­‐state  – GNSS  based,  with  classical  obs.  incl.  in  adjustments  – Did  NOT  use  CORS  as  constraints  

• National  Re-­‐Adjustment  of  2007  – NAD  83(CORS96)  and  (NSRS2007)  – Simultaneous  nationwide  adjustment  (GNSS  only)  

• Latest  realization:  NAD  83(2011)  epoch  2010.00  • NAVD88  realized  in  1989,’93,  ’03,  2009,  2012

Page 15: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

We  calculate  new  positions  from  better,  more,  and  more  recent  measurements,  and  things  “shift”

Page 16: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

NETWORK TIME NETWORK LOCAL SHIFT ACCURACY ACCURACY

NAD 27 1927-1986 10 meter s (1:100,000) 10-200 m

NAD83(86) 1986-1990 1 meter (1:100,000) 0.3-1.0 m

NAD83(199x)* 1990-2007 0.1 meter (1:1 million) 0.05 m “HARN”, “FBN” (1:10 million)

NAD83(NSRS2007) 2007-2011 0.01 meter 0.01 meter 0.03 m

NAD83(NSRS2011) 2011 0.01 meter 0.01 meter 0.01 m

National Spatial Reference System (NSRS) Changes over time

ShiftLocalAccuracy

Page 17: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Practical guide to datum transformations in ESRI’s World

Page 18: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

So  I  need  to  convert  data  between  datums.  What  is  the  best  choice?

NAD27  (or  legacy  datums)  to  NAD83(86)  or  to  NAD83(HARN)    -­‐  Use  NADCON,  a  grid-­‐based  model,  or  local  shia  from  benchmark  

NAD83(86)  to  NAD83(96/2007/2011/HARN)  -­‐  consider  them  equivalent  (1  m  error),  or  local  shia  from  BM.  ARC  DT  DOES  NOTHING!  

NAD83(96)  to  NAD83(2007/2011/HARN)  -­‐  consider  them  equivalent  (10cm),  or  local  shia  from  BM.  ARC  DT  DOES  NOTHING!  

ITRF/WGS84  to  NAD83(all  flavors)  -­‐  find  the  right  serial  set  of  datum  transformahons

Page 19: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

NAD27 to NAD83(86/HARN/96/2007/2011)

Page 20: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

https://desktop.arcgis.com/en/arcmap/latest/map/projections/pdf/geographic_transformations.pdf

ESRI Geographic Transformation Documentation

Page 21: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

NAD27 to NAD83 - Calculated shift at each benchmark, fit a minimum curvature model (local least squares)

Page 22: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Grid-based Model also fit for Longitude NAD27 - NAD83

Page 23: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Not All Grid-based Datum Transformations

Supported

e.g.,

NGZD1949 to NGZD2000

You’re outta luck, at least for now

Page 24: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

e.g., when NAD83(CORS96) data to a NAD83 (86) data frame

results in a warning

Converting Between Flavors of NAD83 (86/HARN/96/2007/2011)

Page 25: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

To Transform between NAD83 versions

Use either a local shift, or consider them equal

ArcGIS applies the transformation below, but with 0 values for T, all R values

+

Page 26: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

+

Effectively, ArcGIS assumes the NAD83 continental versions are all equal, that is

NAD83(86) equals NAD83(96) equals NAD83(2007) equals NAD83(2011)

So in Arc, this continental Datum Transformation makes no difference

Page 27: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Within a single state, there is a HARN grid-based method, so you should use those when converting, but only within a single state

Page 28: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

To Transform between “Early” Earth-Centered Datums, or, Ignoring Continental Drift, Improved Measurements

Use this when transforming between fixed-date WGS84/ITRF and NAD83

Page 29: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Using  published  ITRF00  to  NAD83(96)  R  values  ITRF_2000_To_NAD_1983_CORS96  ITRF_2000_To_NAD_1983_HARN  ITRF_2000_To_NAD_1983_2011  WGS_1984_(ITRF00)_To_NAD_1983_HARN  WGS_1984_(ITRF00)_To_NAD_1983_CORS96  WGS_1984_(ITRF00)_To_NAD_1983_2011  WGS_1984_(ITRF00)_To_NAD_1983  

Using  published  ITRF08  to  NAD83(2011)  R  values  ITRF_2008_To_NAD_1983_2011  WGS84_(ITRF08)_To_NAD_1983_2011  

geodesy.noaa.gov/CORS/coord_info/  coordtrans_no_support_tables.shtml    www.ngs.noaa.gov/CORS/coords.shtml

ESRI  Transformahons  with  Idenhcal  Parameters  

Page 30: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

https://desktop.arcgis.com/en/arcmap/latest/map/projections/pdf/geographic_transformations.pdf

+

Page 31: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

ITRF  (WGS84)  to  NAD83ITRF(20xx)  to  NAD83(86/HARN/96/20072011)  -­‐  find  the  right  serial  chain  of  datum  transformahons  -­‐    

Page 32: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

ITRF  (WGS84)  to  NAD83ITRF(20xx)  to  NAD83(86/HARN/96/20072011)  -­‐  find  the  right  serial  chain  of  datum  transformahons  -­‐    

If  ITRF/WGS84  in  2008,  use  single  published  Datum  Transfrom,  ITRF_2008_To_NAD_1983_2011  

Page 33: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

ITRF  (WGS84)  to  NAD83ITRF(20xx)  to  NAD83(86/HARN/96/20072011)  -­‐  find  the  right  serial  chain  of  datum  transformahons  -­‐    

If  ITRF/WGS84  in  200x,  use  serial  published  DT,  e.g.  ITRF_2000_to_ITRF_2005,  ITRF_2000_to_ITRF_2008 ITRF_2008_To_NAD_1983_2011  

Page 34: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

ITRF  (WGS84)  to  NAD83ITRF(20xx)  to  NAD83(86/HARN/96/20072011)  -­‐  find  the  right  serial  chain  of  datum  transformahons  -­‐    

If  ITRF/WGS84  in  200x,  use  serial  published  DT,  e.g.  ITRF_2000_to_ITRF_2005,  ITRF_2000_to_ITRF_2005 ITRF_2008_To_NAD_1983_2011  

Page 35: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

NAD83(86) to NAD83(CORS96)

Page 36: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

NAD83  to  ITRF,  and  Future  Datums,  We  Must  Add  Time  Component  to  Coordinates  for  Centimeter-­‐level  Accuracies

• your  positional  metadata  should  include:  – datum  – epoch  – source  

• Needed  to  transform  from  current  to  new  datum  • maintaining  your  original  survey  data,  including  date  collected  (epoch)  will  provide  more  accurate  results

Page 37: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

We use our usual equations, but the coefficients of the R matrix are time dependent

Page 38: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Datum Transformation Parameters (R, T) fit for ITRF96 to NAD83(CORS96)

T, v values depend on time since 1997

Page 39: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Four Major “Continental” Horizontal Datums

U.S. & Canada Europe Australia South America

Soler & Marshall

Use Time-adjusted datum transformations between them

Page 40: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

What About the Vertical Height?

e.g., I have data in a 2003 geoid, how do I combine it with 2012B geoid data?

I have heights collected with GPS in an ITRF2008/WGS84 ellipsoid, how do I combine these with NAVD88 data?

Page 41: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Orthometric height measurements always at right angles to each equipotential surface

Page 42: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

Heights are relative to the geoid, XYZ/Lat-Lon-R measured and datum transformed on the ellipsoid…..between

different reference frames and times, both the geoid and the ellipsoid can differ, affecting height

Page 43: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

How Much Does Geoid Differ? Use VDatum

6.5 cm difference

Page 44: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

How Much Does Geoid Differ? Use VDatum

2009 - 1.7 cm 2003 - 7.4 cm 1999 - 6.0 cm 1996 - 6.5 cm

In St Paul, Difference between Geoid 12B and previous datums:

Page 45: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

2009 - 1.7 cm 2003 - 7.4 cm 1999 - 6.0 cm 1996 - 6.5 cm

2012B to:

Page 46: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

From VDatumHeight from NAD83(96) ellipsoid surface to geoid 12B is -27.54 m

Height from WGS84/ITRF08 ellipsoid surface to geoid12B is -28.48 m

Page 47: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

From VDatum, and NOAA Geoid12B Website, Height from NAD83 Ellipsoid and WGS84/ITRF08 Ellipsoid is

0.925 m (WGS84 is above)

So difference between ellipsoids is greater than between geoid versions

Page 48: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

2.2 meters

hNAD83(2011)

hITRF08

ITRF08

NAD83(2011)

surface

What to do? In U.S., biggest difference due to difference in ellipsoid - use Datum

Page 49: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

NAD 83(2011) to IGS08 at epoch 2022.0

Page 50: Datum Evolution - GIS Courses · 2016. 11. 1. · and datum transformed on the ellipsoid…..between different reference frames and times, both the geoid and the ellipsoid can differ,

NAD 83(2011) to IGS08 at epoch 2022.0