1983
DOI: 10.1152/jappl.1983.54.5.1188
|View full text |Cite
|
Sign up to set email alerts
|

Barometric pressures at extreme altitudes on Mt. Everest: physiological significance

Abstract: Barometric pressures were measured on Mt. Everest from altitudes of 5,400 (base camp) to 8,848 m (summit) during the American Medical Research Expedition to Everest. Measurements at 5,400 m were made with a mercury barometer, and above this most of the pressures were obtained with an accurate crystal-sensor barometer. The mean daily pressures were 400.4 +/- 2.7 (SD) Torr (n = 35) at 5,400 m, 351.0 +/- 1.0 Torr (n = 16) at 6,300 m, 283.6 +/- 1.5 Torr (n = 6) at 8,050 m, and 253.0 Torr (n = 1) at 8,848 m. All th… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

3
58
0
2

Year Published

1990
1990
2024
2024

Publication Types

Select...
7
2
1

Relationship

0
10

Authors

Journals

citations
Cited by 116 publications
(63 citation statements)
references
References 5 publications
3
58
0
2
Order By: Relevance
“…Secondly, cooler and denser conditions will increase the partial pressure of oxygen following the ideal gas law (for example, at 6,000 m the change in density altitude by 690 m would increase inspired PO 2 from ∼75-81 mm Hg, or 10-10.8 kPa), increasing the diffusion gradient at the alveoli-blood interface and potentially increasing hemoglobin saturation. This increase may be critical in O 2 uptake, as has been shown for mountaineers attempting to reach the summit of Mount Everest (27) without supplementary oxygen. In addition, early flights would avoid the potential heat load of flying at low altitudes in India during the hottest time of the day, whilst cooler nighttime and early morning temperatures could help dissipate metabolically produced heat from the body (maximum daily temperatures in the Khumbu valley were 23.4°C at 2,660 m, 17.2°C at 3,560 m, and −10°C at 5,585 m).…”
Section: Resultsmentioning
confidence: 79%
“…Secondly, cooler and denser conditions will increase the partial pressure of oxygen following the ideal gas law (for example, at 6,000 m the change in density altitude by 690 m would increase inspired PO 2 from ∼75-81 mm Hg, or 10-10.8 kPa), increasing the diffusion gradient at the alveoli-blood interface and potentially increasing hemoglobin saturation. This increase may be critical in O 2 uptake, as has been shown for mountaineers attempting to reach the summit of Mount Everest (27) without supplementary oxygen. In addition, early flights would avoid the potential heat load of flying at low altitudes in India during the hottest time of the day, whilst cooler nighttime and early morning temperatures could help dissipate metabolically produced heat from the body (maximum daily temperatures in the Khumbu valley were 23.4°C at 2,660 m, 17.2°C at 3,560 m, and −10°C at 5,585 m).…”
Section: Resultsmentioning
confidence: 79%
“…This change is more pronounced at higher latitudes and during the winter [3] and leads to lower inspired oxygen partial pressure, alveolar oxygen partial pressure (PA,O 2 ) and arterial oxygen tension (Pa,O 2 ) values. Air density and ambient temperature also decrease, with the latter falling at a rate of 1uC for every 150-m gain in elevation [4].…”
Section: Environmental Changes At High Altitude That May Affect Pulmomentioning
confidence: 99%
“…Given that flight is a particularly costly form of transport, in terms of the rate of oxygen consumption, and that oxygen becomes progressively more rarefied at higher altitudes, powered flight should become progressively more challenging with altitude. For example, at 8000 m, the minimum mechanical power required for flight is 50 per cent greater than that at sea level [34], whereas the partial pressure of oxygen is 40 per cent lower than that at sea level [35]. The postulated high-altitude migration of bar-headed geese is thus a paradox of avian migration ecology and physiology [17].…”
Section: Introductionmentioning
confidence: 99%