Abstract

Acute mountain sickness (AMS) is a common condition among non-acclimatized individuals ascending to high altitude. However, the underlying mechanisms causing the symptoms of AMS are still unknown. It has been suggested that AMS is a mild form of high-altitude cerebral edema both sharing a common pathophysiological mechanism. We hypothesized that brain swelling and consequently AMS development is more pronounced when subjects exercise in hypoxia compared to resting conditions. Twenty males were studied before and after an eight hour passive (PHE) and active (plus exercise) hypoxic exposure (AHE) (FiO2 = 11.0%, PiO2∼80 mmHg). Cerebral edema formation was investigated with a 1.5 Tesla magnetic resonance scanner and analyzed by voxel based morphometry (VBM), AMS was assessed using the Lake Louise Score. During PHE and AHE AMS was diagnosed in 50% and 70% of participants, respectively (p>0.05). While PHE slightly increased gray and white matter volume and the apparent diffusion coefficient, these changes were clearly more pronounced during AHE but were unrelated to AMS. In conclusion, our findings indicate that rest and especially exercise in normobaric hypoxia are associated with accumulation of water in the extracellular space, however independent of AMS development. Thus, it is suggested that AMS and HACE do not share a common pathophysiological mechanism.

Highlights

  • Acute mountain sickness (AMS) constitutes a widespread medical condition among un-acclimatized individuals ascending to high altitude (.2500 m) too fast

  • We hypothesized that brain swelling and AMS development is more pronounced when subjects exercise in hypoxia compared to resting conditions

  • AMS during passive hypoxic exposure (PHE) and 10 had only minor symptoms that did not fulfill the criteria for AMS

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Summary

Introduction

Acute mountain sickness (AMS) constitutes a widespread medical condition among un-acclimatized individuals ascending to high altitude (.2500 m) too fast. A prevailing hypothesis points to a pathophysiological process within the central nervous system suggesting that AMS is a self-limiting mild form of HACE (high altitude cerebral edema) both sharing a common pathophysiological mechanism. AMS may be considered an early stage of subclinical brain edema leading to intracranial hypertension and the symptoms of AMS [5]. This hypothesis has been supported by two recently published magnetic resonance imaging (MRI) studies (1.5 and 3.0 Tesla) which provided convincing evidence for mild vasogenic brain swelling in subjects with (AMS+) and without AMS (AMS2) following 6–18 h passive exposure to normobaric hypoxia (FiO2,12%). Cytotoxic (intracellular) edema was detected only in AMS+

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