Critical Environmental Limits for Human Thermoregulation in the Context of a Changing Climate.

Exercise, sport, & movement Pub Date : 2023-01-01 Epub Date: 2023-04-11 DOI:10.1249/esm.0000000000000008
Daniel J Vecellio, Rachel M Cottle, S Tony Wolf, W Larry Kenney
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Abstract

Human-caused climate change has increased the average temperature of the Earth by over 1°C since the 19th century with larger increases expected by 2100 due to continued human influence. This change in mean ambient temperature has had nonlinear effects, resulting in more high temperature extremes, i.e., heat waves, that have increased in frequency, duration, and magnitude. Additional occurrences of humid heatwaves have significantly affected human health due to the physiological strain associated with a relative inability for evaporative cooling. Inability to efficaciously cool the body, whether during passive heat exposure or physical activity, not only leads to elevated core temperatures but also places strain on the cardiovascular system, often exacerbating age-related co-morbidities. As part of the PSU HEAT (Pennsylvania State University - Human Environmental Age Thresholds) Project, a progressive environmental strain protocol has been developed to determine critical environmental limits - combinations of ambient temperature and humidity -- associated with uncompensable heat stress and intractable rises in core temperature (Tc). These human heat balance thresholds, well below those originally theorized by climatologists, have been surpassed in recent heatwaves and be exceeded on a more regular basis in the future, providing additional impetus to the urgency of adaptative measures and climate change mitigation.

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气候变化背景下人类体温调节的关键环境极限
自 19 世纪以来,人类造成的气候变化使地球平均气温上升了 1°C 以上,由于人类的持续影响,预计到 2100 年会有更大幅度的上升。平均环境温度的这种变化产生了非线性影响,导致更多的极端高温,即热浪,其频率、持续时间和强度都有所增加。更多的潮湿热浪严重影响了人类的健康,这是因为相对无法蒸发冷却所造成的生理压力。无论是在被动受热还是在体力活动时,如果身体无法有效降温,不仅会导致核心温度升高,还会给心血管系统造成压力,往往会加重与年龄有关的并发症。作为宾夕法尼亚州立大学人类环境年龄阈值项目(PSU HEAT)的一部分,我们制定了一个渐进式环境应变协议,以确定临界环境极限(环境温度和湿度的组合),这些极限与难以承受的热应激和核心温度(Tc)难以控制的升高有关。这些人类热平衡阈值远远低于气候学家最初的理论值,在最近的热浪中已经被超过,并且在未来会更经常地被超过,这进一步推动了适应措施和减缓气候变化的紧迫性。
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