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This document explores the physiological responses of humans to extreme conditions such as high altitudes and cold environments. It explains how the atmosphere affects the ability to survive at high elevations due to cold temperatures, low humidity, and reduced oxygen levels. The mechanisms of homeostasis, thermoregulation, and the impacts of hypoxia are detailed, alongside the body's responses to cold stress and inadequate oxygen supply. Additionally, adaptations such as increased insulation and heat production are discussed, providing insight into the survival strategies of warm-blooded mammals in harsh climates.
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Man at High Altitudes • Atmosphere controls ability to live at high altitudes • Cold temperature • Low humidity • Low oxygen
Physiological Responses to Cold Environments • Homeostasis- Warm-blooded mammals maintain a relatively constant body temperature regardless of ambient conditions- humans 37oC • Homeostasis achieved by control mechanisms that regulate heat production and loss • Core body temperature drop of a few degrees reduces enzymatic activity, coma, death • Core body temperature increases of a few degrees may irreversibly damage the central nervous system • C Van Wie (1974) Physiological response to cold environments. Arctic & Alpine Enviornments
Adaptation to Cold Environments • To maintain temperature: • Increase insulation • Increase heat production • Lower core temperature (hypothermia)
Thermoregulation • Heat produced by metabolic processes and muscular exertion • Inactive • Brain 16% • Chest and abdomen 56% • Skin and muscles 18% • Active • Brain 3% • Chest and abdomen 22% • Skin and muscles 73%
Thermoregulation • Heat lost from body core to muscle and skin by conduction and convection • Blood circulating through body carries heat from core to outer body • Some lost to air • Much of the heat transferred to cooler veinous blood returning from extremities • Enables body to maintain extremities at lower temperature
Skin layer heat losses • As air flow increases, convective heat loss from skin increases- windchill • Evaporation • Predominant heat loss from skin in cold environments is radiation • Nude, with skin temp 31C, radiates 116 Watts to room with walls of 21C • At rest, total heat production is 84 Watts • Better put some clothes on
Wind Chill Science • http://windchill.ec.gc.ca/workshop/index_e.html? • http://windchill.ec.gc.ca/workshop/papers/html/session_2_paper_1_e.html • Bluestein, Maurice, Jack Zecher, 1999: A New Approach to an Accurate Wind Chill Factor. Bulletin of the American Meteorological Society: Vol. 80, No. 9, pp. 1893–1900.
Pathologic Effects of Excessive Heat Loss • If skin temperature < freezing for extended period: • Chilblains- red, swollen itching lesions between joints of fingers • Trench foot- similar to chilblains except on foot • If skin freezes • Frostbite- local burning and stinging followed by numbness • Exposure- condition when body is not able to maintain a normal temperature • Core temp < 30C lose consciousness • Core temp < 27C heart ceases
Physiological Response to Cold Stress • Autonomic control measures respond to cold by: • Increasing heat production • Increasing insulation layers • Permit moderate hypothermia (lower core body temperature)
Heat Generation • At rest, muscles provide 18% of total heat • Voluntary exercise- heat production increased 10 times • Involuntary exercise- shivering • heat production increased 4-5 times • but 90% of heat produced by shivering lost by convection because of body movements • Non-shivering thermogenesis • Metabolism/hormones of body adjust and increase heat production
Insulation • Initial reaction to cold • Blood vessels in extremities contract rapidly • Increases insulation of body • Long term- more fat
Physiological Factors of Altitude: Oxygen Deficiency • Proportion of Oxygen in atmosphere- 21% • Partial pressure of Oxygen decreases with height in proportion to other gases • Lungs saturated with water vapor; reduces available oxygen • Oxygen in lungs: (ambient pressure – saturation water vapor pressure at body temp (37C) (63 mb)) * .21 • Sea level (1013 – 63 ) * .21 = 200 mb; 5000 m (540 – 63 ) * .21 = 100 mb • Hypoxia- intolerance to oxygen deficiency • Humans can tolerate half sea level value indefinitely • Symptoms significant above 3000 m (133 mb of Oxygen) • Standard Atmosphere varies with latitude (4000 m roughly 630 mb equatorward of 30o; 593 mb (winter)-616 mb (summer) at 60o • Cyclone could drop pressure 10-20 mb; equivalent to several hundred meters in elevation • Grover (1974); Man living at high altitudes. Arctic and Alpine Environments.
Inspired Oxygen as a Function of Elevation 200mb 100mb
Supplemental Oxygen • Mt. Everest (8848 m/29,028 ft) • Mean pressure near 314 mb • Most climbers use bottled oxygen above 7300 m (24,000 ft) • Pilots required to use supplemental oxygen above 3810 m (12,500 ft) for flights lasting more than 30 minutes
Oxygen in the body • PIO2- inspired oxygen- oxygen available in the lungs • O2 transported in body by respiratory pigment haemoglobin in red blood cells • Lungs oxygenate blood • Heart pumps blood through body • High pressure of O2 in capillaries causes diffusion into tissue • Sea-level- 100 ml of blood contains 20 ml of O2
Physiological Adaptions to Hypoxia • Reduced PIO2 reduces pressure of O2 in blood: PaO2 • Brain triggers respiratory muscles to bring greater volume of air into lungs with each breath • Hyperventilation- increase volume of air inspired per minute offsets decrease in air density • # O2 molecules taken into lungs per minute is nearly same as at sea level • However, while quantity of O2 available in lungs remains unchanged, PaO2 reduced as elevation increases • Reduced PaO2 haemoglobin binds less O2; less saturation of O2 in blood; reduces O2 in blood
Oxygen Saturation 70 116 mb
Other physiological changes • Decrease in Oxygen in blood causes heart rate to increase initially in order to maintain Oxygen transport • Amount of water in blood plasma decreases after about a week • Decreases plasma volume without changing volume of red blood cells • Blood can carry greater quantity of Oxygen • Prolonged hypoxia stimulates bone marrow to produce more red blood cells • After a week, heart rate normalizes but stroke volume (volume pumped by left ventricle) decreases, leading to net drop in cardiac oxygen output
VO2 • Highest pressure in O2 transport system determines efficiency of system • VO2- aerobic working capacity- maximum amount of O2 that can be consumed per minute • 10% decrease in VO2 per 1000m increase in altitude above 1500 m • Humans can’t work as hard at high elevation as at lower ones
Problems at High Altitude • Humans can adapt to altitudes of 3-4 km and remain healthy indefinitely • Acute mountain sickness- initial response to rapid ascent to high elevation • Poor sleep; headaches; nausea; vomiting; apathetic; irritable; little appetite • Chronic mountain sickness- develops in people who have lived at high elevation for years; lose adaptation to hypoxia • Pulmonary Oedema • Accumulation of fluids in the lungs interrupts transfer of oxygen from air to blood
Athletic Use of Hypoxia http://www.sltrib.com/2001/aug/08262001/sports/126267.htm