Barometric Altimetry Using the Vernier LabPro. Purpose of Report Improved altitude determination for Balloon Fest and other activities Improved altitude.

Slides:



Advertisements
Similar presentations
Chapter 8 Air pressure and winds.
Advertisements

CHAPTER Continuity The tangent line at (a, f(a)) is used as an approximation to the curve y = f(x) when x is near a. An equation of this tangent.
Investigating HVAC’s Effect on Barometer Readings indoors Wonsang Song.
Class #5: Air pressure and winds Chapter 8 1Class #5 Tuesday, July 13, 2010.
ATMO 336 Weather, Climate and Society Surface and Upper-Air Maps.
Part 6. Altimetry. Part 6. Altimetry TOPICS Pressure, Humidity & Temperature ISA and the Aircraft Altimeter 4 Pressure, Humidity & Temperature 4 ISA.
Aviation Weather Hazards: Density Altitude
What Makes the Wind Blow? ATS 351 Lecture 8 October 26, 2009.
Earth and Atmospheric Sciences EAS535 Atmospheric Measurements and Observations II EAS 535
Skip to Navigation Skip to Content. Variation of Air Pressure with Altitude.
1 NATS 101 Lecture 3 Climate and Weather. 2 Review and Missed Items Pressure and Height-Exponential Relationship Temperature Profiles and Atmospheric.
Section 03 - Altimetry Lesson 08
Meteorology 5.02 Pressure References: FTGU pages 127 Air Command Weather Manual.
AIR PRESSURE Keeping an Atmosphere Atmosphere is kept by the world’s gravity –Low mass (small) worlds= low gravity =almost no atm. –High mass (large)
Air Pressure - #1 element of weather prediction.
Pressure Sensors Absolute – A Sensor That Measures Input Pressure in Relation to a Zero Pressure. We Will Use the Absolute Pressure Sensor to Calculate.
Classification of Instruments :
Atmospheric Measurements Nick Bassill January 28 th 2009.
GASES Chapter 10 Gravity pulls the air molecules toward the earth, giving them weight. The weight of the air molecules all around us is called the.
ME 322: Instrumentation Lecture 5 January 28, 2015 Professor Miles Greiner Lab 3, transmitter characteristics, least-squares, standard error of the estimate.
Ch 3 – Pressure, Altitude & Density
Air Pressure By: The Furry Ewoks Orcutt Academy Ty Fredriks.
Weather Part IV Storms Reference: CK-12.org Earth Sciences Chapter 16 By: Robert Smith.
Pressure. The amount of force an object puts on a surface. Pressure is measured by a barometer. Atmospheric pressure comes from air being pulled down.
Judah Levine, NIST, Mar-2006: 1 Using g to monitor the snow pack Judah Levine John Wahr Department of Physics University of Colorado
OCTOBER 20 AIM: What is PRESSURE ? Atmospheric pressure Units Gas pressure.
NATS 101 Lecture 2 Vertical Structure of the Atmosphere.
Section 02 Lesson 5/6/7 Atmospheric Pressure, Temperature and Density
Section 03 - Altimetry (cont) Lesson 09
Statistics for Managers Using Microsoft Excel, 4e © 2004 Prentice-Hall, Inc. Chap 6-1 Chapter 6 The Normal Distribution and Other Continuous Distributions.
Performance characteristics for measurement and instrumentation system
Chapter 3 The Changing Weather. Chapter 3 Terms Condensation Condensation Orographic Condensation Orographic Condensation Convectional Condensation Convectional.
GASES THE THIRD STATE OF MATTER We live at the bottom of an ocean of air – the ATMOSPHERE The highest pressures occur at the lowest altitudes. If you.
Air Pressure and Winds. Atmospheric Pressure  What causes air pressure to change in the horizontal?  Why does the air pressure change at the surface?
Reading a Station Model from a Weather map. Cold Fronts & Warm Fronts.
Chapter 6: Air Pressure and Winds Atmospheric pressure Atmospheric pressure Measuring air pressure Measuring air pressure Surface and upper-air charts.
Lecture I Sensors.
An example of vertical profiles of temperature, salinity and density.
Dr. Kamel Mohamed Guedri Umm Al-Qura University, Room H1091
OBJ: Given notes and activity sheets SWBAT construct and interpret isoline maps such as a weather map with 70% accuracy. DN: Copy notes ACT: Introduction.
Aviation Seminars1 #3259. What is pressure altitude? A- The indicated altitude corrected for position and installation error. B- The altitude indicated.
Chapter 2 Describing Motion: Kinematics in One Dimension.
ATM OCN 100 Summer ATM OCN 100 – Summer 2004 LECTURE 2B ATMOSPHERIC PRESSURE: A Fundamental Weather Element (con’t.) u A. Practical Problem u B.
Pressure Basics  Force per unit area  Barometric/ Air/ Atmospheric pressure is the force exerted by air molecules –Nitrogen (78%) –Oxygen (21%) –Water.
ATM OCN 100 Summer ATM OCN 100 – Summer 2002 LECTURE 4 ATMOSPHERIC PRESSURE: A Fundamental Weather Element (con’t.) u A. Practical Problem u B.
1 ATMOSPHERIC PRESSURE & DENSITY. 2 The denser the atmosphere…  the greater its weight, and  the greater its air pressure.
 The condition of Earth’s atmosphere at a particular time and place.
Instrument Characteristics  Scientific Instrument: l A device for making a measurement.  Measurement: l An action intended to assign a number as the.
Palm trees feeling the push of the air from a hurricane wind A balloon is inflated from a CO2 canister; pressure is increasing as the balloon inflates.
Chapter 5 Air Pressure. Driving Question What is the significance of horizontal and vertical variations in air pressure?
The Course of Synoptic Meteorology
Weather Lesson Two Pressure and Wind.
MECH 373 Instrumentation and Measurement
Station vs. MSL Pressure
Weather 101 and beyond Edward J. Hopkins
Air Pressure Can you feel it?.
Air Pressure Air molecules are moving constantly
Meterology The study of atmospheric phenomena
Upper Air Data The Atmosphere is 3D and can not be understood or forecast by using surface data alone.
Air Pressure Can you feel it?.
Gases Boyle’s Law.
Gas Variables.
AIM: What are the general properties of gases and what is PRESSURE
Air Pressure Can you feel it? 1.
Weather Stations and Weather Maps
5.02 Pressure References: FTGU pages 127 Air Command Weather Manual
Air Pressure Can you feel it? 1.
ALTIMETRY.
Aim: How can we explain air pressure?
AIR PRESSURE.
Presentation transcript:

Barometric Altimetry Using the Vernier LabPro

Purpose of Report Improved altitude determination for Balloon Fest and other activities Improved altitude determination for Balloon Fest and other activities Determine characteristics of Vernier Barometer sensor Determine characteristics of Vernier Barometer sensor –Resolution –Uncertainty –Accuracy Establish reliable procedures for testing and use. Establish reliable procedures for testing and use.

Barometer Sensor Specs Sensitivity: V/atm Sensitivity: V/atm Digital resolution: mBar (~0.8m) Digital resolution: mBar (~0.8m)

Atmospheric Pressure Profile Standard Atmosphere Model 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)

Converting Sensor output to Altitude Data Sensor Output SlopeIntercept Volts m/V m kPa m/kPa m Atm m/Atm m In Hg m/inHg 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 kPa.

Dynamic Pressure Effects Difference of pressure (  P) on the leading edge of a body moving through air with a relative velocity (v):  P= ½ v 2  Difference of pressure (  P) on the leading edge of a body moving through air with a relative velocity (v):  P= ½ v 2  Error in altitude determination due to dynamic pressure:  H =  P  84 m/kPa Error in altitude determination due to dynamic pressure:  H =  P  84 m/kPa At 10 MPH:  H = 1 m At 10 MPH:  H = 1 m At 60 MPH:  H = 36 m At 60 MPH:  H = 36 m

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

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 2:30pm 6/9/07

Summary of Observations Warm up: 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) Sensors outputs vary by up to 0.4 kPa (~35 m) Read about 1 kPa (9m) higher than official sources. Read about 1 kPa (9m) higher than official sources. Have a digital resolution of about 0.8 m. Have a digital resolution of about 0.8 m. Random variations of about ± 2 steps Random variations of about ± 2 steps Uncertainty (std deviation) of ± 1.6 m. Uncertainty (std deviation) of ± 1.6 m.

Conclusion Relative altimetry is possible to an accuracy of 2 or 3 meters if painstaking effort is taken to eliminate or mathematically remove: 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)