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High Altitude Pulmonary Edema

High altitude pulmonary edema is a noncardiogenic pulmonary edema that develops after rapid ascent to over 2500 m (usually over 3000 m) in unacclimatized people. It is the commonest cause of death from altitude illness.

Incidence is 0.2% in visitors going to 4500 m over 4 or more days, and up to 6% after rapid ascent to 5500 m.

The risk is greater with fast ascent, heavy exertion, cold, previous episodes (a 60% recurrence rate on repeated rapid ascent) and, in children, with respiratory infection. People living at altitude can develop it on returning from a low-altitude stay (re-entry edema).

Mechanism: alveolar hypoxia causes exaggerated and uneven hypoxic pulmonary vasoconstriction. Pulmonary artery pressure rises to over 40 mmHg, and areas of lung that are over-perfused develop high capillary pressure, leading to stress failure of the capillary wall with leakage of protein-rich fluid and red cells into alveoli. Impaired alveolar fluid clearance and a reduced hypoxic ventilatory response contribute. Pulmonary edema in these patients is patchy and inflammatory changes follow.

Symptoms start 2 to 4 days after arrival, often at night. Untreated mortality is up to 50%, and with early descent and oxygen it is under 5%. Complications: respiratory failure, high altitude cerebral edema (coexisting in about 14 to 50% of fatal cases), pulmonary infection and recurrence on reascent.

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