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Individual variation in response to altitude training
Abstract
Moderate-altitude living (2,500 m), combined with low-altitude training (1,250 m) (i.e., live high-train low), results in a significantly greater improvement in maximal O 2 uptake (V˙o 2 max ) and performance over equivalent sea-level training. Although the mean improvement in group response with this “high-low” training model is clear, the individual response displays a wide variability. To determine the factors that contribute to this variability, 39 collegiate runners (27 men, 12 women) were retrospectively divided into responders ( n = 17) and nonresponders ( n = 15) to altitude training on the basis of the change in sea-level 5,000-m run time determined before and after 28 days of living at moderate altitude and training at either low or moderate altitude. In addition, 22 elite runners were examined prospectively to confirm the significance of these factors in a separate population. In the retrospective analysis, responders displayed a significantly larger increase in erythropoietin (Epo) concentration after 30 h at altitude compared with nonresponders. After 14 days at altitude, Epo was still elevated in responders but was not significantly different from sea-level values in nonresponders. The Epo response led to a significant increase in total red cell volume andV˙o 2 max in responders; in contrast, nonresponders did not show a difference in total red cell volume or V˙o 2 max after altitude training. Nonresponders demonstrated a significant slowing of interval-training velocity at altitude and thus achieved a smaller O 2 consumption during those intervals, compared with responders. The acute increases in Epo and V˙o 2 max were significantly higher in the prospective cohort of responders, compared with nonresponders, to altitude training. In conclusion, after a 28-day altitude training camp, a significant improvement in 5,000-m run performance is, in part, dependent on 1) living at a high enough altitude to achieve a large acute increase in Epo, sufficient to increase the total red cell volume andV˙o 2 max , and 2) training at a low enough altitude to maintain interval training velocity and O 2 flux near sea-level values.
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“Irrespective of the hypoxic strategy adopted, a reduction in arterial O2 content, induced by either a reduction in the partial pressure of O2 (hypobaric hypoxia) or a direct reduction of O2 concentration (normobaric hypoxia), triggers the activation of hypoxia‐inducible factor‐1α (Semenza, 2000), subsequently leading to an increased erythropoietic response (Montero & Lundby, 2019) and rising haem”
From Effect of live‐high, train‐low strategy induced by chronic low‐dose carbon monoxide exposure on haematological parameters and performance in trained individuals (2026) · cites this paper as Chapman et al., 1998
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Cited by
Genetic Evidence for High-Altitude Adaptation in Tibet
Simonson, T. S., Yang, Y., Huff, C. D., Yun, H., Qin, G., Witherspoon, D. J., Bai, Z., Lorenzo, F. R., Xing, J., Jorde, L. B., et al. (2010) · Science · doi:10.1126/science.1189406 · Cited by 1,227
Jones, A. M. (2014) · Applied Physiology, Nutrition, and Metabolism · doi:10.1139/apnm-2014-0036 · Cited by 144
Wang, J., Ji, Y., Zhou, L., Xiang, Y., Heinonen, I., & Zhang, P. (2019) · Frontiers in Physiology · doi:10.3389/fphys.2019.00701 · Cited by 22
Villanova, S., Porcelli, S., Ekström, L., & Cardinale, D. A. (2026) · Experimental Physiology · doi:10.1113/ep093005 · Cited by 5
Metadata
- Authors
- Chapman, R. F., Stray-Gundersen, J., & Levine, B. D.
- Affiliations
- Institute for Exercise and Environmental Medicine, Presbyterian Hospital of Dallas, Dallas 75231; and University of Texas Southwestern Medical Center, Dallas, Texas 75235
- Venue
- Journal of Applied Physiology
- Publisher
- American Physiological Society
- Published
- 1998-10-01
- Volume
- 85
- Issue
- 4
- Pages
- 1448-1456
- ISSN
- 8750-7587
- 1522-1601
- Cited by
- 283
- References
- 0
- Language
- en
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