Rapid ascent to high altitude (2500m or more) can result in the development in High Altitude Pulmonary Oedema (HAPE). Discuss the aetiology and the pathophysiology of HAPE.

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Rapid ascent to high altitude (2500m or more) can result in the development in High Altitude Pulmonary Oedema (HAPE). Discuss the aetiology and the pathophysiology of HAPE.

In recent years mountain climbing and mounting trekking has grown in popularity, however there are certain dangers associated with high altitude (2500m or higher) pursuits. It has been known for centuries that there are risks of damaged health to humans by going to high altitudes; with the physiological effects of being at altitude being realised since the 19th century. It has also been known that these effects are as a result of inspiring less oxygen as there is a fall in barometric pressure with altitude (Sonna, 2002) (Figure 1).

(Figure 1). Shows the fall in barometric pressure and PO2 associated with a rise in  

                  altitude.

(Lumb, 2000).

As seen from viewing figure 1, both the barometric pressure and inspired PO2 dramatically decrease with an increase in altitude. From sea level (0 m) to 3000m (the typical altitude HAPE develops at) there is a decrease from 760 mmHg to 520 mmHg for barometric pressure, a 140 mmHg / 18.5 % decrease. Inspired PO2 values decrease from 150 mmHg to 100 mmHg, a 50 mmHg / 33.3 % decrease. It is this decrease in oxygen inspiration that causes physiological problems associated with high altitudes.

There are relatively few physiological problems associated with altitudes under 2000m and most problems do not manifest themselves until altitudes of over 3000m, however if a rapid ascent is made then problems can occur at, or less than 2500m (Eccles, 2000; Kumar and Clark, 1998). Some common problems associated with high altitudes especially after rapid ascent and not allowing for acclimatisation include, headache, depressed urine output, light-headedness, dyspnea, insomnia, dimness of vision, weakness, irritability and nausea, these are collectively known as Acute Mountain Sickness (AMS). Many people develop AMS (Figure 2), which can be easily treated by a decrease in altitude and pure oxygen inspiration, as long as climbers are in groups and well educated of such conditions there are relatively few serious outcomes from AMS (McArdle et al., 1996; Taylor et al., 1989). There is however a far more serious less common condition (Figure 2), it is called High Altitude Pulmonary Oedema (HAPE).

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Acclimatisation can be termed as changes in metabolism and physiology in order to withstand the new conditions (McArdle et al., 1996).

(Sonna, 2002).

As can be seen from figure 2 the number of people who contract AMS is high with a mean value of 49.5 % ± 14.6 %, however the number of people who then develop   HAPE is relatively low at 2.5 % ± 1.9 %.  

High altitude pulmonary oedema (HAPE) is a subject that has grown in interest in the past 15 years as more people are getting into situations where they may ...

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