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AMBIENT TEMPERATURE CHANGES
     AND THE IMPACT TO
  TIME MEASUREMENT ERROR
Vukan Ogrizović, Jelena Gučević, Siniša Delčev
           University of Belgrade
           Faculty of Civil Engineering
           Department of Geodesy and Geoinformatics
Vertical deflections

      Natural coordinates (Φ,Λ)   Elipsoidal coordinates (φ,λ)
           - astronomical -               - geodetic -
Φ 5 = const.                      φ5 = const.
Φ 4 = const.                      φ4 = const.

Φ 3 = const.                      φ3 = const.

Φ s = const.                      φs = const.
                         ξ = Φ − φ = const.
                                  φ
Φ1 = const.                         1


                         η = ( Λ − λ ) cos φ
                     A − α = ( Λ − λ ) sin φ
Measuring systems for
          (Φ,Λ) determination
         TZK2 - D                    DIADEM
(Institut für Erdmessung,   (Eidgenössishe Technische
        Hannover)               Hochschule, Zürich)
Time-keeping in field
• 1PPS from GPS to DB9 via RS232
• GPST to quartz oscillator ticks
• RTOS
Frequency vs temperature plots
• Variations in temperature -> major influence on the
  crystal frequency
• Changing the curvature of a crystal cut can make the
  slope less steep
Experiment set-up
•   Time reference: Trimble NetRS w Zephyr Geodetic
•   UTC source: 1PPS output (BNC type) wired to DB9
•   SI second acquisition: Interrupt handler under RTOS
•   Resolution:
      133 MHz ≈ 7 ⋅10 −9 s
Set-up #1
                 - Testing performed outdoors
                 - Ambient temperature: ~17°C
                 - Measuring session: ~2 h



Raw data




After removing the blunders
Set-up #2
              - Testing at different environmental conditions
              - Ambient temperature increased from 0°C to 21°C
              - Measuring session: ~5 h



Raw data




After removing the blunders
  Set-up 2a                 Set-up 2c                     Set-up 2b
Calculation of the clock model
• Four tests, each cca 2 h long:
  – #1:    T = 17°C
  – #2a:   T = 0°C
  – #2b:   T = 21°C
  – #2c:   0°C < T < 21°C
• Clock drift & bias according to the linear
  model:
      UTCi = T0 + (1 + h )Ti
Calculated biases (tab'd)
Set-up #       T [ °C]   h [s/h]   sh [s/h]
   1             16       0,003     0,001
  2a             0       -0,033     0,002
  2b             20       0,006     0,002
  2c           0-21      -0,026     0,003
Calculated biases (graph)
Conclusion and remarks
• Clock bias strogly dependent on temperature
• Need for stable environmental conditions
• Shorter session -> linear clock model
Thank you for your attention!
   University of Belgrade
   Faculty of Civil Engineering
   Department of Geodesy and Geoinformatics




   Vukan Ogrizović, vukan@grf.bg.ac.rs
   Jelena Gučević, jgucevic@grf.bg.ac.rs
   Siniša Delčev, delcev@grf.bg.ac.rs

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Ambient Temperature Changes and the Impart to Time Measurement Error

  • 1. AMBIENT TEMPERATURE CHANGES AND THE IMPACT TO TIME MEASUREMENT ERROR Vukan Ogrizović, Jelena Gučević, Siniša Delčev University of Belgrade Faculty of Civil Engineering Department of Geodesy and Geoinformatics
  • 2. Vertical deflections Natural coordinates (Φ,Λ) Elipsoidal coordinates (φ,λ) - astronomical - - geodetic - Φ 5 = const. φ5 = const. Φ 4 = const. φ4 = const. Φ 3 = const. φ3 = const. Φ s = const. φs = const. ξ = Φ − φ = const. φ Φ1 = const. 1 η = ( Λ − λ ) cos φ A − α = ( Λ − λ ) sin φ
  • 3. Measuring systems for (Φ,Λ) determination TZK2 - D DIADEM (Institut für Erdmessung, (Eidgenössishe Technische Hannover) Hochschule, Zürich)
  • 4. Time-keeping in field • 1PPS from GPS to DB9 via RS232 • GPST to quartz oscillator ticks • RTOS
  • 5. Frequency vs temperature plots • Variations in temperature -> major influence on the crystal frequency • Changing the curvature of a crystal cut can make the slope less steep
  • 6. Experiment set-up • Time reference: Trimble NetRS w Zephyr Geodetic • UTC source: 1PPS output (BNC type) wired to DB9 • SI second acquisition: Interrupt handler under RTOS • Resolution: 133 MHz ≈ 7 ⋅10 −9 s
  • 7. Set-up #1 - Testing performed outdoors - Ambient temperature: ~17°C - Measuring session: ~2 h Raw data After removing the blunders
  • 8. Set-up #2 - Testing at different environmental conditions - Ambient temperature increased from 0°C to 21°C - Measuring session: ~5 h Raw data After removing the blunders Set-up 2a Set-up 2c Set-up 2b
  • 9. Calculation of the clock model • Four tests, each cca 2 h long: – #1: T = 17°C – #2a: T = 0°C – #2b: T = 21°C – #2c: 0°C < T < 21°C • Clock drift & bias according to the linear model: UTCi = T0 + (1 + h )Ti
  • 10. Calculated biases (tab'd) Set-up # T [ °C] h [s/h] sh [s/h] 1 16 0,003 0,001 2a 0 -0,033 0,002 2b 20 0,006 0,002 2c 0-21 -0,026 0,003
  • 12. Conclusion and remarks • Clock bias strogly dependent on temperature • Need for stable environmental conditions • Shorter session -> linear clock model
  • 13. Thank you for your attention! University of Belgrade Faculty of Civil Engineering Department of Geodesy and Geoinformatics Vukan Ogrizović, vukan@grf.bg.ac.rs Jelena Gučević, jgucevic@grf.bg.ac.rs Siniša Delčev, delcev@grf.bg.ac.rs