Variation in barometric pressure in Melbourne does not significantly affect the BTPS correction factor.
The conventional BTPS (body temperature and pressure, saturated with water vapour) correction factor varies with ambient barometric pressure (P(B)) and many lung function laboratories measure P(B) daily. The aim was to investigate whether a fixed value for P(B) could replace daily measurements. P(B) was measured daily over a 12-month period. The highest and lowest values in Melbourne in the last century were also recorded from data published by the Bureau of Meteorology. Using these P(B) values, the BTPS factor was determined for a range of spirometer temperatures and compared to the BTPS factors obtained using a fixed ambient pressure of 101.3 kPa. The mean (SD) P(B) measured over the 12-month period was 102.2 kPa (0.64) with a range of 99.9-103.6 kPa. The level of disagreement between the BTPS factor calculated using a P(B) of 101.3 kPa instead of the measured value was greater at lower temperatures. Over the extremes of P(B) during the last century (98.0-104.3 kPa) the use of a standard pressure (101.3 kPa) produced an error in the BTPS factor of </= 0.16%. Daily variations in P(B) do not significantly affect the magnitude of the conventional BTPS correction factor and a fixed value, such as 101.3 kPa at sea level, can be used with little error.
Johns
David P
DP
Discipline of Medicine, University of Tasmania, Hobart, Tasmania, Australia. David.Johns@utas.edu.au
Hartley
M Faizel
MF
Burns
Graham
G
Thompson
Bruce R
BR
D001274:Atmospheric Pressure; D001831:Body Temperature; D006801:Humans; D013147:Spirometry / Q000592:standards*; D014739:Victoria