GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4...

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EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS-specific local effects at the Geodetic Observatory Wettzell Peter Steigenberger, Urs Hugentobler, Ralf Schmid Technische Universität München (TUM) Manuela Seitz Deutsches Geodätisches Forschungsinstitut (DGFI), München Uwe Hessels, Thomas Klügel Bundesamt für Kartographie und Geodäsie (BKG), Geodetic Observatory Wettzell

Transcript of GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4...

Page 1: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

GNSS-specific local effects at the Geodetic Observatory Wettzell

Peter Steigenberger, Urs Hugentobler, Ralf SchmidTechnische Universität München (TUM)

Manuela SeitzDeutsches Geodätisches Forschungsinstitut (DGFI), München

Uwe Hessels, Thomas KlügelBundesamt für Kartographie und Geodäsie (BKG), Geodetic Observatory Wettzell

Page 2: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

Motivation and Outline

Local tie height discrepancies at Wettzell from DTRF2008

GPSVLBI

GPSSLR

GPSGPS

Outline

• GNSS network at Wettzell

• GNSS processing

• Frequency-dependent systematic effects on station coordinates

• Residual maps

• igs08.atx receiver antennacalibrations

• Conclusions

Page 3: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

Local Surveys

WTZR

WTZA

Horizontal displacement Vertical displacement

1 mm

Vertical displacement

WTZTWTZRWTZJWTZAWTZZWTZL

The precision of the local ties in Wettzell is at the 1-2 mm level

Page 4: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

GNSS Sites at Wettzell

WTZRWTZZWTZA WTZJ

WTZRWTZZWTZA

Data analyzed from 329/1997 – 57/2011

Page 5: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

GNSS Processing• Double difference solution with Bernese 5.1, IGS05 reference

frame, igs05.atx antenna model• WTZA as reference: no antenna change, no discontinuities• Reprocessed (1997 – 2008) and operational (2009 – 2011) CODE

products:- Satellite orbits and Earth rotation parameters

• Estimation of troposphere parameters for all stations but WTZA- Zenith delays with 2h parameter spacing, VMF1, ECMWF- One pair of east-west and north-south gradients per day- Elevation-dependent weighting: cos2z

• Ambiguity fixing for L1 and L2 with Sigma method, mean resolution rate of 99.5%

• Computation of L1, L2, and L3 (ionosphere-free) solutions

Page 6: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

WTZR w.r.t. WTZA with Troposphere Estimation

L1 L2 L3

Antenna change Local Tie

Page 7: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

WTZR w.r.t. WTZA with Troposphere Estimation

L1 L2 L3

Antenna change Local Tie

Microwave absorberplate installed

Page 8: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

Cumulative Solution: Height Component

WTZJ WTZR WTZZWTZT

Differences between baseline w.r.t. WTZA and local tieTroposphere parameters estimated

L1 L2 L3

Page 9: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

Cumulative Solution: Height Component

WTZJ WTZR WTZZWTZT

Uncalibrated Radome

Differences between baseline w.r.t. WTZA and local tieTroposphere parameters estimated

L1 L2 L3

Page 10: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

Impact of Troposphere Estimation

WTZJ WTZR WTZZWTZT

L3 station height discrepancies with and without troposphere estimation

Page 11: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

Troposphere Zenith Delays for WTZR

Page 12: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

L3 Troposphere BiasesTr

opos

pher

eB

ias

[mm

]

WTZJ WTZR WTZT WTZZ

Mean bias and standard deviation per solution interval (due to antenna changes) for ionosphere-free linear combination

Page 13: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

Estimation of Residual Maps

• Local ties fixed• No elevation-dependent

weighting, 10° cut-off • L3 residuals for WTZT with

uncalibrated radome

WTZT, September 1998 (uncalibrated radome)

Page 14: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

WTZT with uncalibrated radome

Application of Residual Maps

uncorrected withouttroposphere estimation

uncorrected withtroposphere estimation

residual-corrected withouttroposphere estimation

residual-corrected withtroposphere estimation

zenith-dependent corrections from September 1998 applied

L3 S

olut

ion

ΔU

p [m

m]

1998

Mar MayJan SepJul

Page 15: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

Residual Maps: WTZR

September 2010LEIAR25.R3 LEIT

September 2009LEIAR25 LEIT

September 2008AOAD/M_T NONE

Residuals [mm]

Page 16: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

igs08.atx Receiver Antenna Calibrations

Differences to station heights derived with igs05.atx receiver calibrations

Updated robot calibration New robot calibration

Agr

eem

ent w

ith lo

cal t

ies

Deg

rade

dIm

prov

ed

WTZJ WTZR WTZZWTZT

L1 L2 L3

Page 17: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011

Summary and Conclusions

• Precision of the local ties at Wettzell is at the 1-2 mm level

• L1, L2, and L3 GPS solutions differ by up to 5 cm• L3 differences w.r.t. local ties can reach the cm level• Discrepancies are caused by GPS, not the local tie measurements• Discrepancies amplified by estimation of troposphere parameters

• Near-field effects like multipath are most likely the source for these frequency-dependent systematic effects

• Residual maps show systematic effects at the cm level• Residual maps could be used for differential corrections (w.r.t.

reference site or previous antenna at same site)

• Should such corrections be applied within the IGS?

Page 18: GNSS-specific local effects at the Geodetic Observatory ... · EGU General Assembly 2011, Wien, 4 – 8 April 2011 GNSS Processing • Double difference solution with Bernese 5.1,

EGU General Assembly 2011, Wien, 4 – 8 April 2011