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Unlabelled: Singh, G.K., Mahendra Singh Deora, Rajan Grewal, A. Kushwaha, and Sukhmeet Minhas. Is high altitude a risk factor in development of herpes zoster? High Alt Med Biol. 19:244-248, 2018.
Background: Old age immune-compromised states are known to increase the risk of herpes zoster (HZ). The aim of this study was to find out whether arrival into high altitude poses a risk for the development of HZ in lowlanders.
Methods: A retrospective study of 173 cases of HZ was carried out between January 1, 2005 and December 31, 2010 in people working at high altitude areas of Leh. Data of lowlander people working at high altitude were compared with that of high altitude native and similar group of people working at plains during the same period.
Results: HZ constitutes 2.36% (95% confidence interval [CI], 2.04-2.73) of total skin outpatient department cases at a hospital at high altitude, whereas it was 0.23% (95% CI, 0.18-0.29) at a tertiary hospital at plains. In lowlanders working at high altitude, frequency of herpers zoster varied between 2.63% and 3.59% with mean of 3.07%. Frequency of HZ in persons presenting to a tertiary dermatological center at plains varied from 0.19% to 0.26% (mean of 0.23%). Presence of high altitude posed a risk of almost seven times in developing HZ in comparison with its absence with odds ratio of 7.21 and 95% CI varying from 5.42 to 9.60. This result was statistically very significant with p value <0.0001.
Conclusions: Lowlanders working at high altitude are at high risk to develop HZ in comparison with persons working at plains. However, a large population-based study is required to investigate and establish the same.
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http://dx.doi.org/10.1089/ham.2018.0005 | DOI Listing |
Am J Physiol Regul Integr Comp Physiol
September 2025
United States Army Research Institute of Environmental Medicine, Natick, MA, US.
Unlabelled: Insulin resistance has been associated with acute mountain sickness (AMS) risk, but the influence of active ascent is unclear.
Methods: Thirty-two unacclimatized Soldiers (23±4yr; 80±14 kg) were tested at baseline residence (BLR), hiked ~5 km (n=16) or were driven (n=16) to 4,300 m, and stayed for 4 days (~66 h). Venous blood was taken each morning at BLR and during high altitude (HA) exposure days 2-4 (HA2-4) and the evening on day 1 at HA (HA1).
PLoS One
September 2025
Misión Biológica de Galicia (MBG-CSIC), Pontevedra, Galicia, Spain.
Specialized plant metabolism, particularly phenolic compound production, contributes significantly to the functioning and resilience of mountain ecosystems. Livestock grazing can influence phenolic production, with its effects varying depending on microclimatic factors and soil conditions. Despite the ecological significance of this process, the impact of livestock grazing on phenolic production in alpine plants remains insufficiently explored.
View Article and Find Full Text PDFExp Physiol
September 2025
Department of Sports Science and Clinical Biomechanics, Faculty of Health Sciences, University of Southern Denmark, Odense, Denmark.
High-altitude training is widely adopted by endurance athletes with the aim of increasing total haemoglobin mass (tHb) and thereby endurance exercise performance. However, divergent effects on tHb and exercise performance have been reported in athletes commencing altitude camps with initial high baseline levels for tHb, questioning the efficacy of in-season interventions in elite athletes. Therefore, haematological adaptations and exercise performance were evaluated in 12 elite cyclists completing an in-season 'Live High-Train High' (LHTH) altitude camp (21 days at 3000 m) immediately after participating in the national championships.
View Article and Find Full Text PDFPLoS One
September 2025
Comet Research Group, Prescott, Arizona, United States of America.
Shocked quartz grains are an accepted indicator of crater-forming cosmic impact events, which also typically produce amorphous silica along the fractures. Furthermore, previous research has shown that shocked quartz can form when nuclear detonations, asteroids, and comets produce near-surface or "touch-down" airbursts. When cosmic airbursts detonate with enough energy and at sufficiently low altitude, the resultant relatively small, high-velocity fragments may strike Earth's surface with high enough pressures to generate thermal and mechanical shock that can fracture quartz grains and introduce molten silica into the fractures.
View Article and Find Full Text PDFFront Immunol
August 2025
Azienda Sanitaria Territoriale Fermo, Fermo, Italy.