High Altitude Cerebral Edema
High altitude cerebral edema is a life-threatening encephalopathy that develops in the setting of acute mountain sickness, as the severe end of a continuum, usually at over 4000 m and after 2 or more days at altitude. Incidence is 0.5 to 1% of climbers at 4000 to 5000 m, and higher over 5500 m. It is defined by ataxia and altered mental status in a person with recent ascent, with or without symptoms of acute mountain sickness.
Mechanism: hypoxemia causes cerebral vasodilation and raises cerebral blood flow and capillary pressure. Vasogenic edema follows from disruption of the blood-brain barrier by hypoxia-induced mediators (vascular endothelial growth factor, nitric oxide and free radicals), and cytotoxic edema contributes later.
The raised intracranial pressure and the white matter involvement (particularly the corpus callosum, the splenium in particular) cause the ataxia and confusion.
Magnetic resonance imaging shows hemosiderin deposits from microhemorrhages that persist for years in survivors.
Without treatment, coma and death follow within 24 hours of the onset of ataxia. With early descent, most patients recover, but deficits (ataxia, cognitive impairment) can persist for weeks. High altitude pulmonary edema coexists in about half of cases. Complications: coma, herniation, seizures (uncommon), retinal hemorrhage, cranial nerve palsies and persistent cognitive deficits.













