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1 a highly depleted layer inferred from thermo-barometric analysis of xenoliths.
2 laboratory data across diverse hydrothermal, barometric, and lithological conditions, we demonstrate
3 ness to inhaled methacholine was assessed by barometric body plethysmography, and numbers of lung eos
4 ness to inhaled methacholine was assessed by barometric body plethysmography, and numbers of lung eos
5 rical analysis, we demonstrate that a single barometric component with seasonally modulated amplitude
6 ning multidirectional muographic images with barometric data, we anticipate that muography will becom
7 O(2) into vapour bubbles, producing spurious barometric estimates.
8 alysis that indicates that there is a set of barometric frequencies, consistent with the inverse nume
9   Room temperature isotherms are obtained by barometric measurements in an accurately calibrated stir
10         Ventilation was determined using the barometric method, and oxygen consumption and CO(2) prod
11                                        Using barometric plethysmography to measure respiratory functi
12          Our results show that in whole-body barometric plethysmography, hM3Dq-mediated, global Foxb1
13  was assessed by a combination of whole-body barometric plethysmography, invasive measurement of airw
14 at high altitude (Cerro de Pasco (CP), Peru; barometric pressure (P(B)) 450 mmHg) and repeated, follo
15 workload with acute compression to sea level barometric pressure (SL) and acute decompression to 5000
16 el data and (2) using the combined data with barometric pressure as an independent variable.
17   An alternative strategy is to increase the barometric pressure as in aircraft cabins.
18                                      The low barometric pressure at high altitude causes lower arteri
19 ted with surface-level relative humidity and barometric pressure but not associated with wind conditi
20 ing strategies do not consider the effect of barometric pressure changes on gas migration and may not
21  gas emissions can be directly influenced by barometric pressure changes.
22          Regional temperature, humidity, and barometric pressure data from automated monitors were us
23                            At high altitude, barometric pressure falls and with it inspired P(O2), po
24                                              Barometric pressure has a substantial effect; PCO2, base
25 ta constraining ground-level air density and barometric pressure have been reported, leaving the plau
26 rcise at 760 Torr (SL) and at 410 Torr (ALT) barometric pressure in a pressure chamber.
27  measurements per second and compensates for barometric pressure in real time.
28                             The inclusion of barometric pressure in the equations allows better predi
29  oscillatory flow at the seabed) than either barometric pressure or bottom water temperature, two cov
30     At sea level, the equation that included barometric pressure predicted Pa(O(2)) slightly better t
31 s, higher wind speeds, and greater change in barometric pressure than Townsend's big-eared bats.
32 l-delay maps of observational field data for barometric pressure to demonstrate the structure of lati
33 ments were consistent with the TC trails and barometric pressure variations observed at meteorologica
34 at 8400 m (27,559 ft)--at which altitude the barometric pressure was 272 mm Hg (36.3 kPa)--the mean P
35 ure, precipitation, humidity, wind speed and barometric pressure) we first identify the sentiment and
36 read, with an evident decline in wind speed, barometric pressure, and latent heat flux.
37 e adjusted for day of the week, temperature, barometric pressure, and relative humidity.
38  effects of temperature and humidity), time, barometric pressure, day of the week, and particulate ma
39                                  The reduced barometric pressure, oxygen pressure, and air density, t
40 an environmental source of stress--plausibly barometric pressure--might be responsible for the annual
41 ta such as temperature, solar irradiance and barometric pressure.
42 spired Po(2), which is caused by the reduced barometric pressure.
43 thway (a few microseconds) and variations in barometric pressure.
44 2 was calculated by multiplying FECO2 by the barometric pressure.
45 ed with relative humidity and 24-h change in barometric pressure.
46                                 Decreases in barometric-pressure led to surface gas breakthroughs (>2
47                 We demonstrate that although barometric pressures are complicated signals comprised o
48 who travel to terrestrial altitudes at which barometric pressures are the same as those in commercial
49  adult volunteers to determine the effect of barometric pressures equivalent to terrestrial altitudes
50 ns unclear whether prolonged exposure to low barometric pressures exacerbates SCD aetiologies or impa
51  of the post-detonation chimney coupled with barometric pumping produced a synergistic effect amplify
52 ver pressuring of the detonation cavity, and barometric pumping while gas sorption, dissolution, radi
53 set of dominant gas transport frequencies in barometric records.
54                               An elementary "barometric" relation for the driving force is introduced
55  metabolic cage studies, blood gas analysis, barometric respirometry, perfusion of isolated cortical
56 approximates gas transport due to a measured barometric signal.
57                                      If past barometric tendencies are expected to continue at a loca
58 o consider stochastic realizations of future barometric variations.
59                                        Using barometric whole-body plethysmography and increases in e
60 measurement of AR to inhaled methacholine by barometric whole-body plethysmography is a valid indicat