Partial Pressure of Arterial Oxygen in Healthy Adults at High Altitudes: A Systematic Review and Meta-Analysis

Importance: With increasing altitude, the partial pressure of inspired oxygen decreases and, consequently, the Pao$_{2}$ decreases. Even though this phenomenon is well known, the extent of the reduction as a function of altitude remains unknown. Objective: To calculate an effect size estimate for the decrease in Pao$_{2}$ with each kilometer of vertical gain among healthy unacclimatized adults and to identify factors associated with Pao$_{2}$ at high altitude (HA). Data Sources: A systematic search of PubMed and Embase was performed from database inception to April 11, 2023. Search terms included arterial blood gases and altitude. Study Selection: A total of 53 peer-reviewed prospective studies in healthy adults providing results of arterial blood gas analysis at low altitude (<1500 m) and within the first 3 days at the target altitude (≥1500 m) were analyzed. Data Extraction and Synthesis: Primary and secondary outcomes as well as study characteristics were extracted from the included studies, and individual participant data (IPD) were requested. Estimates were pooled using a random-effects DerSimonian-Laird model for the meta-analysis. Main Outcomes and Measures: Mean effect size estimates and 95% CIs for reduction in Pao$_{2}$ at HA and factors associated with Pao$_{2}$ at HA in healthy adults. Results: All of the 53 studies involving 777 adults (mean [SD] age, 36.2 [10.5] years; 510 men [65.6%]) reporting 115 group ascents to altitudes between 1524 m and 8730 m were included in the aggregated data analysis; 13 of those studies involving 305 individuals (mean [SD] age, 39.8 [13.6] years; 185 men [60.7%]) reporting 29 ascents were included in the IPD analysis. The estimated effect size of Pao$_{2}$ was −1.60 kPa (95% CI, −1.73 to −1.47 kPa) for each 1000 m of altitude gain (τ$^{2}$ = 0.14; I$^{2}$ = 86%). The Pao$_{2}$ estimation model based on IPD data revealed that target altitude (−1.53 kPa per 1000 m; 95% CI, −1.63 to −1.42 kPa per 1000 m), age (−0.01 kPa per year; 95% CI, −0.02 to −0.003 kPa per year), and time spent at an altitude of 1500 m or higher (0.16 kPa per day; 95% CI, 0.11-0.21 kPa per day) were significantly associated with Pao$_{2}$. Conclusions and Relevance: In this systematic review and meta-analysis, the mean decrease in Pao$_{2}$ was 1.60 kPa per 1000 m of vertical ascent. This effect size estimate may improve the understanding of physiological mechanisms, assist in the clinical interpretation of acute altitude illness in healthy individuals, and serve as a reference for physicians counseling patients with cardiorespiratory disease who are traveling to HA regions

Exercise Performance in Central Asian Highlanders: A Cross-Sectional Study

Forrer, Aglaia, Philipp M. Scheiwiller, Maamed Mademilov, Mona Lichtblau, Ulan Sheraliev, Nuriddin H. Marazhapov, Stéphanie Saxer, Patrick Bader, Paula Appenzeller, Shoira Aydaralieva, Aybermet Muratbekova, Talant M. Sooronbaev, Silvia Ulrich, Konrad E. Bloch, and Michael Furian. Exercise performance in central Asian highlanders: A cross-sectional study. High Alt Med Biol. 22:386-394, 2021. Introduction: Life-long exposure to hypobaric hypoxia induces physiologic adaptations in highlanders that may modify exercise performance; however, reference data for altitude populations are scant. Methods: Life-long residents of the Tien Shan mountain range, 2,500 - 3,500 m, Kyrgyzstan, free of cardiopulmonary disease, underwent cardiopulmonary cycle exercise tests with a progressive ramp protocol to exhaustion at 3,250 m. ECG, breath-by-breath pulmonary gas exchange, and oxygen saturation by pulse oximetry (SpO2) were measured. Results: Among 81 highlanders, age (mean ± SD) 48 ± 10 years, 46% women, SpO2 at rest was 88% ± 2%, peak oxygen uptake (V'O2peak) was 21.6 ± 5.9 mL/kg/min (76% ± 15% predicted for a low-altitude reference population); peak work rate (Wpeak) was 117 ± 37 W (77% ± 17% predicted), SpO2 at peak was 84% ± 5%, heart rate reserve (220 - age - maximal heart rate) was 28 ± 17/min, ventilatory reserve (maximal voluntary ventilation - maximal minute ventilation) was 68 ± 32 l/min, and respiratory exchange ratio was 1.03 ± 0.09. Peak BORG-CR10 dyspnea and leg fatigue scores were 5.1 ± 2.0 and 6.3 ± 2.1. In multivariable linear regression analyses, age and sex were robust determinants of Wpeak, V'O2peak, and metabolic equivalent (MET) at peak, whereas body mass index, resting systolic blood pressure, and mean pulmonary artery pressure were not. Conclusions: The current study shows that V'O2peak and Wpeak of highlanders studied at 3,250 m, near their altitude of residence, were reduced by about one quarter compared with mean predicted values for lowlanders. The provided prediction models for V'O2peak, Wpeak, and METs in central Asian highlanders might be valuable for comparisons with other high altitude populations. Keywords: altitude; cardiopulmonary exercise test; high altitude pulmonary hypertension; hypoxia