Barometric Altimetry Using the Vernier LabPro - PowerPoint PPT Presentation

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Barometric Altimetry Using the Vernier LabPro

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Title: Barometric Altimetry Using the Vernier LabPro


1
Barometric AltimetryUsing the Vernier LabPro
2
Purpose of Report
  • Improved altitude determination for Balloon Fest
    and other activities
  • Determine characteristics of Vernier Barometer
    sensor
  • Resolution
  • Uncertainty
  • Accuracy
  • Establish reliable procedures for testing and
    use.

3
Barometer Sensor Specs
  • Sensitivity 13.08 V/atm
  • Digital resolution 0.003 mBar (0.8m)

4
Atmospheric Pressure Profile
  • Standard Atmosphere Model

Near sea level, this exponential model yields
almost identical results as the Adiabatic,
Constant Temperature, and Meteorological models
do. We can assume that over a small change of
altitude (i.e. 1000ft) this exponential curve
approximates a straight line. However, the slope
of this linear approximation changes
significantly as one moves to higher ground
altitudes (e.g. 15 difference in slope between
0 ft and 6000 ft)
5
Converting Sensor output to Altitude Data
Sensor Output Slope Intercept
Volts -659.3 m/V 1635 m
kPa -84.50 m/kPa 8560 m
Atm -8562 m/Atm 8560 m
In Hg -24.96 m/inHg 8560 m
Slope is calculated from US Standard Atmosphere
Model for elevations between 1000 and 2000 ft
above sea level. The Intercept is based on sea
level pressure being 101.3 kPa.
6
Dynamic Pressure Effects
  • Difference of pressure (?P) on the leading edge
    of a body moving through air with a relative
    velocity (v) ?P ½ v2 ?
  • Error in altitude determination due to dynamic
    pressure ?H ?P?84 m/kPa
  • At 10 MPH ?H 1 m
  • At 60 MPH ?H 36 m

7
Field Tests
  • USGS topo maps typically 20 ft contours
  • Google Earth appears good but has unknown
    accuracy
  • Weather services report three kinds of pressure
  • Station, Barometric, Altimeter

8
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9
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10
Barometric Pressure during the Accuracy and Drift
Test as reported at SLO airport about 9 miles
north of test location at an elevation of 212 ft
MSL. This graph covers the time from 2pm 6/8/07
thru 230pm 6/9/07
11
Summary of Observations
  • Warm up
  • Time from 2 minutes to as much as 1 hour.
  • Increasing pressure from 0.1 kPa to as much as
    1.3 kPa
  • Decreasing error in altitude measurement from 8
    m to as much as 110 m.
  • Sensors outputs vary by up to 0.4 kPa (35 m)
  • Read about 1 kPa (9m) higher than official
    sources.
  • Have a digital resolution of about 0.8 m.
  • Random variations of about 2 steps
  • Uncertainty (std deviation) of 1.6 m.

12
Conclusion
  • Relative altimetry is possible to an accuracy of
    2 or 3 meters if painstaking effort is taken to
    eliminate or mathematically remove
  • warm-up drift
  • Pressure drift (weather changes)
  • Dynamic pressure effects (due to wind or motion)
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