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1 a highly depleted layer inferred from thermo-barometric analysis of xenoliths.
2 ness to inhaled methacholine was assessed by barometric body plethysmography, and numbers of lung eos
3 ness to inhaled methacholine was assessed by barometric body plethysmography, and numbers of lung eos
4   Room temperature isotherms are obtained by barometric measurements in an accurately calibrated stir
5         Ventilation was determined using the barometric method, and oxygen consumption and CO(2) prod
6                                        Using barometric plethysmography to measure respiratory functi
7  was assessed by a combination of whole-body barometric plethysmography, invasive measurement of airw
8 at high altitude (Cerro de Pasco (CP), Peru; barometric pressure (P(B)) 450 mmHg) and repeated, follo
9 el data and (2) using the combined data with barometric pressure as an independent variable.
10   An alternative strategy is to increase the barometric pressure as in aircraft cabins.
11                                      The low barometric pressure at high altitude causes lower arteri
12          Regional temperature, humidity, and barometric pressure data from automated monitors were us
13                            At high altitude, barometric pressure falls and with it inspired P(O2), po
14                                              Barometric pressure has a substantial effect; PCO2, base
15 ta constraining ground-level air density and barometric pressure have been reported, leaving the plau
16  measurements per second and compensates for barometric pressure in real time.
17                             The inclusion of barometric pressure in the equations allows better predi
18     At sea level, the equation that included barometric pressure predicted Pa(O(2)) slightly better t
19 l-delay maps of observational field data for barometric pressure to demonstrate the structure of lati
20 at 8400 m (27,559 ft)--at which altitude the barometric pressure was 272 mm Hg (36.3 kPa)--the mean P
21 e adjusted for day of the week, temperature, barometric pressure, and relative humidity.
22  effects of temperature and humidity), time, barometric pressure, day of the week, and particulate ma
23 an environmental source of stress--plausibly barometric pressure--might be responsible for the annual
24 thway (a few microseconds) and variations in barometric pressure.
25 2 was calculated by multiplying FECO2 by the barometric pressure.
26 spired Po(2), which is caused by the reduced barometric pressure.
27 who travel to terrestrial altitudes at which barometric pressures are the same as those in commercial
28  adult volunteers to determine the effect of barometric pressures equivalent to terrestrial altitudes
29                               An elementary "barometric" relation for the driving force is introduced
30                                        Using barometric whole-body plethysmography and increases in e
31 measurement of AR to inhaled methacholine by barometric whole-body plethysmography is a valid indicat

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