Atmospheric pressure and altitude relationship help

Pressure with Height: pressure decreases with increasing altitude

atmospheric pressure and altitude relationship help

Atmospheric pressure and inspired oxygen pressure fall roughly linearly with It may help match ventilation and perfusion within the lung, but in hypoxia of. By Bogna Haponiuk. If you ever wondered what is the atmospheric pressure high up in the mountains, our air pressure at altitude calculator is there to help you. As the elevation increases from sea level the atmospheric pressure decreases. and advanced life support | Atmospheric pressure is a variable that has been.

Heart The heart works remarkably well at altitude. Initially there is an increase in cardiac output in relation to physical work but later this settles to sea level values. At all times there is increased heart rate and decreased stroke volume for a given level of work, though the maximum obtainable heart rate falls as higher altitudes are reached.

Brain Hypoxia has progressive effects on the functioning of the central nervous system. Accidents that occur at extreme altitude on Everest and other mountains may be due to poor judgment as a consequence of hypoxic depression of cerebral function. More worrying is that these effects on cerebral function may be permanent.

Oxygen at high altitude

The American Medical Research Expedition to Everest studied its climbers a year after return to sea level and found some enduring abnormalities of cognitive function and ability to perform fast repetitive movements, although most functions tested had returned to pre-expedition values. Blood Initially on travelling to altitude haemoglobin concentrations rise through a fall in the plasma volume due to dehydration. The increased viscosity of the blood coupled with increased coagulability increases the risk of stroke and venous thromboembolism.

Some authors advocate regular venesection in high altitude climbs; others recommend prophylactic aspirin. Neither has been shown scientifically to reduce the incidence of venous or arterial thrombosis. Acclimatisation Adequate acclimatisation is essential for safe travelling in the mountains.

At altitudes above m individuals should climb no more than m per day with a rest day every third day.

A small experiment visualizing atmospheric pressure at different altitudes.

Anyone suffering symptoms of acute mountain sickness should stop, and if symptoms do not resolve within 24 hours descend at least m. There can be a tendency, particularly on commercial expeditions, to push on at a rate that is too fast for weaker members of the group.

This is dangerous, and the rate of ascent should be set to that of the slowest members of the party. Recognising altitude related illness Acute mountain sickness Acute mountain sickness is self limiting and usually affects previously healthy individuals who go too rapidly to altitude. There may be no symptoms for the first hours. Thereafter symptoms develop and usually peak on the second or third day.

Symptoms include headache, anorexia, insomnia, and breathlessness. The cause of acute mountain sickness is not understood but is clearly related to hypoxia and factors such as effort, air temperature, previous viral respiratory tract infection, and innate susceptibility.

The incidence is quite high.

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High altitude pulmonary oedema This life threatening condition may or may not be preceded by symptoms of acute mountain sickness. Breathlessness increases progressively accompanied by a cough productive of white sputum, which is occasionally tinged with blood.

atmospheric pressure and altitude relationship help

Examination will reveal cyanosis and a mild fever no more than Left untreated this condition can progress rapidly and be fatal. During the debate over the harmful effects of chlorofluorocarbons CFCs on stratospheric ozone, some not-so-reputable scientists claimed that CFCs could not possibly reach the stratosphere because of their high molecular weights and hence low scale heights.

In reality, turbulent mixing of air ensures that CFC mixing ratios in air entering the stratosphere are essentially the same as those in surface air. Exercise The cruising altitudes of subsonic and supersonic aircraft are 12 km and 20 km respectively.

What is the relative difference in air density between these two altitudes? The air density at 20 km is only a third of that at 12 km.

ABC of oxygen: Oxygen at high altitude

The high speed of supersonic aircraft is made possible by the reduced air resistance at 20 km. Consider a coastline with initially the same atmospheric temperatures and pressures over land L and over sea S. Assume that there is initially no wind. In summer during the day the land surface is heated to a higher temperature than the sea.

This difference is due in part to the larger heat capacity of the sea, and in part to the consumption of heat by evaporation of water.

atmospheric pressure and altitude relationship help

Compensating vertical motions result in the circulation cell shown in Figure