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Variation in barometric pressure in Melbourne does not significantly affect the BTPS correction factor
David P Johns1, M Faizel Hartley, Graham Burns
1Discipline of Medicine, University of Tasmania, Hobart, Tasmania, Australia. David.Johns@utas.edu.au
Summary
Daily barometric pressure (P(B)) variations do not significantly impact the body temperature and pressure, saturated with water vapour (BTPS) correction factor. A fixed P(B) value, like 101.3 kPa, can be used in lung function testing with minimal error.
Area of Science:
- Pulmonary Physiology
- Medical Instrumentation
Background:
- The body temperature and pressure, saturated with water vapour (BTPS) correction factor is crucial for accurate lung function testing.
- This factor conventionally varies with ambient barometric pressure (P(B)), necessitating daily P(B) measurements in many laboratories.
Purpose of the Study:
- To evaluate if a fixed barometric pressure (P(B)) value can replace daily measurements for BTPS correction.
- To determine the potential error introduced by using a standard P(B) instead of daily measurements.
Main Methods:
- Daily P(B) was recorded over a 12-month period in Melbourne.
- Historical P(B) extremes from the Bureau of Meteorology were analyzed.
- BTPS factors were calculated using measured P(B) and a fixed P(B) of 101.3 kPa across various spirometer temperatures.
Main Results:
- The mean P(B) over 12 months was 102.2 kPa (SD 0.64), with a range of 99.9-103.6 kPa.
- Disagreement in BTPS factors was slightly greater at lower spirometer temperatures when using a fixed P(B).
- Using a standard P(B) of 101.3 kPa resulted in a maximum error of ≤0.16% even across extreme historical P(B) values (98.0-104.3 kPa).
Conclusions:
- Daily variations in ambient barometric pressure (P(B)) have a negligible impact on the BTPS correction factor.
- A fixed P(B) value, such as 101.3 kPa, is suitable for routine use in lung function laboratories, simplifying procedures and reducing potential errors.