Cold-induced vasodilation and vasoconstriction in the finger of tropical and temperate indigenes

While heat acclimatization reflects the development of heat tolerance, it may weaken an ability to tolerate cold. The purpose of this study was to explore cold-induced vasodilation (CIVD) responses in the finger of tropical indigenes during finger cold immersion, along with temperate indigenes. Thirteen tropical male indigenes (subjects born and raised in the tropics) and 11 temperate male indigenes (subjects born and raised in Japan and China) participated. Subjects immersed their middle finger at 4.3±0.8 °C water for 30 min. Rectal temperature, skin temperatures, finger skin blood flow, blood pressure and subjective sensations were recorded during the test. The results showed that: (1) the tropical group demonstrated a lower minimum (T_min), maximum (T_max) and mean finger temperature (T_mean) compared to those of the temperate group (P<0.05); (2) seven tropical indigenes demonstrated a late-plateau type of CIVD pattern, which is characterized by a pronounced 1st vasoconstriction and a single CIVD with a faint and weak 2nd vasoconstriction, whereas no temperate indigene demonstrated the late-plateau type; and (3) the hand temperature at the end of finger immersion was 3 °C lower in the tropical than the temperate group (P<0.05). These results indicate that tropical indigenes have less active responses of arterio-venous anastomoses in the finger and weaker vasoconstrictions after the first CIVD response during finger cold immersion, which can be considered as being more vulnerable to cold injury of the periphery in severe cold.     

Reproducibility of the cold-induced vasodilation response in the human finger.

Cold-induced vasodilation (CIVD) is a cyclic oscillation in blood flow that occurs in the extremities on cold exposure and that is likely associated with reduced risk of cold injury (e.g., frostbite) as well as improved manual dexterity and less pain while working in the cold. The CIVD response varies between individuals, but the within-subject reproducibility has not been adequately described. The purpose of this study was to quantify the within-subject variability in the CIVD response under standardized conditions. Twenty-one volunteers resting in a controlled environment (27 degrees C) immersed the middle finger in warm water (42 degrees C) for 15 min to standardize initial finger temperature and then in cold water (4 degrees C; CWI) for 30 min, on five separate occasions. Skin temperature (Tf) and blood flow (laser-Doppler; expressed as percent change from warm-water peak) responses that describe CIVD were identified, including initial nadir reached during CWI, onset time of CIVD, initial apex during CIVD, time of that apex, and overall mean during CWI. Within-subject coefficient of variation for Tf across the five tests for the nail bed and pad, respectively, were as follows: nadir, 9 and 21%; onset, 18 and 19%; apex, 12 and 17%; apex time, 23 and 24%; mean 10 and 15%. For blood flow, these values were as follows: nadir 52 and 64%; onset, 6 and 5%; apex, 33 and 31%; apex time 9 and 8%; and mean 43 and 34%. Greater variability was found in the temperature response of the finger pad than the nail bed, but for blood flow the variability was similar between locations. Variability in onset and apex time between sites was similar for both temperature and blood flow responses. The reproducibility of the time course of CIVD suggests this methodology may be of value for further studies examining the mechanism of the response.     

The effect of repeated mild cold water immersions on the adaptation of the vasomotor responses

There are several types of cold adaptation based on the alteration of thermoregulatory response. It has been thought that the temperature of repeated cold exposures during the adaptation period is one of the factors affecting the type of cold adaptation developed. This study tested the hypothesis that repeated mild cold immersions would induce an insulative cold adaptation but would not alter the metabolic response. Seven healthy male participants were immersed to their xiphoid process level repeatedly in 26°C water for 60 min, 3 days every week, for 4 weeks. During the first and last exposure of this cold acclimation period, the participants underwent body immersion tests measuring their thermoregulatory responses to cold. Separately, they conducted finger immersion into 5°C water for 30 min to assess their cold-induced vasodilation (CIVD) response before and after cold acclimation. During the immersion to xiphoid process, participants showed significantly lower mean skin temperature and skin blood flow in the forearm post-acclimation, while no adaptation was observed in the metabolic response. Additionally, blunted CIVD responses were observed after cold acclimation. From these results, it was considered that the participants showed an insulative-type of cold acclimation after the repeated mild cold immersions. The major finding of this study was the acceptance of the hypothesis that repeated mild cold immersion was sufficient to induce insulative cold adaptation but did not alter the metabolic response. It is suggested that the adaptation in the thermoregulatory response is specific to the response which is repeatedly stimulated during the adaptation process.     

Respiratory changes due to extreme cold in the Arctic environment

Effects of acute exposure and acclimatisation to cold stress on respiratory functions were investigated in healthy tropical Indian men (n=10). Initial baseline recordings were carried out at Delhi and thereafter serially thrice at the arctic region and once on return to Delhi. For comparison the respiratory functions were also evaluated on Russian migrants (RM;n=7) and Russian natives (RN;n=6). The respiratory functions were evaluated using standard methodology on a Vitalograph: In Indians, there was an initial decrease in lung vital capacity (VC), forced vital capacity (FVC), forced expiratory volume 1st s (FEV1), peak expiratory flow rate (PEFR) and maximum voluntary ventilation (MVV) on acute exposure to cold stress, followed by gradual recovery during acclimatisation for 4 weeks and a further significant improvement after 9 weeks of stay at the arctic region. On return to India all the parameters reached near baseline values except for MVV which remained slightly elevated. RM and RN showed similar respiratory functions at the beginning of acute cold exposure at the arctic zone. RN showed an improvement after 10 weeks of stay whereas RM did not show much change. The respiratory responses during acute cold exposure are similar to those of initial altitude responses.     

Sleep patterns at an altitude of 3500 metres

Alterations in sleep pattern during acclimatisation at an altitude of 3500 m were studied on 27 healthy men (20–30 years of age). Of these, 15 were sojourners (SJ), 6 were acclimatised lowlanders (AL) and 6 were high altitude natives (HAN). Baseline sleep profile of SJ was electrophysiologically monitored, initially at Delhi (260 m) and later at 3500 m altitude in Western Himalayas for 2 weeks. At high altitude (HA) the sleep patterns of AL and HAN were also monitored for comparison. There were 4 cases of acute mountain sickness (AMS) among SJ, whose sleep profiles were also recorded. The state of autonomic arousal was assessed by a battery of indices, while the psychological arousal was measured by the anxiety scales. On completion of studies at HA, the SJ were flown back to the plains and re-tested within one week of return. SJ showed curtailment of slow wave sleep (SWS) and frequent short episodes of arousal during sleep at HA. AL and HAN also had lesser amounts of SWS; however, the arousals and awakenings during sleep were less frequent. Subjects who experienced AMS had normal amounts of SWS at HA. There was sympathetic hyperactivity and slight increase in anxiety level in SJ, while HAN and AL had relatively reduced level of sympathetic activity. The curtailment of SWS and frequent arousals observed in SJ during the initial phase of acclimatisation at HA, appear to be adaptive features to prevent the accentuation of arterial hypoxemia due to sleep hypoventilation.     

Chemoreceptor sensitivity and maladaptation to high altitude in man

Studies were carried out to find out the role of chemoreceptor sensitivity in the causation of maladaptation syndromes on acute exposure to altitude. The experiments were done in two phases. In phase I, the responses in chemoreceptor sensitivity were studied in altitude acclimatized subjects and compared with those who suffered from either High Altitude Pulmonary Oedema (HAPO) or Acute Mountain Sickness (AMS). In Phase II, a similar comparison was done in two groups of subjects, one representing normal sojourners at 3,500 m and the other being subjects who had just recovered from HAPO. The first phase was done at Delhi; and the second at an altitude of 3,500 m. Parameters of assessment were hypoxic sensitivity, carbon dioxide sensitivity, ventilation (VE), respiratory frequency (Rf), forced vital capacity (FVC), forced expiratory volume at the first second (FEV1), heart rate (HR), blood pressure (BP), and oral temperature (Tor). The results showed significantly lower sensitivity to both hypoxia and carbon dioxide in maladapted subjects, as compared to those who were acclimatized in both the categories suggesting thereby that reduced chemoreceptor sensitivity might be an initiating factor in the causation of maladaptation syndromes at altitude.     

Cold-induced vasodilatation of finger and maximal oxygen consumption of young female athletes born in Hokkaido

To determine whether there is a direct correlation between endurance capacity and cold tolerance, maximal oxygen consumption (VO₂max), and cold-induced vasodilatation (CIVD), we measured these factors in 14 young female athletes born in Hokkaido, Japan's northernmost island. We determined the VO₂max by a standard incremental test on a cycle ergometer and measured the oxygen consumption (VO₂) by means of the Douglas-bag method. We determined the CIVD reaction by measuring the skin temperature of the left middle finger during immersion in cold water at 0°C for 20 min. The athletes showed significant positive correlations between VO₂max, expressed as l/min, and CIVD as well as other peripheral cold tolerance indexes (resistance index against frostbite and CIVD index). The body weight VO₂max (VO₂max/kg body weight) failed to correlate significantly with either the CIVD or with other cold tolerance indexes. These results suggest that CIVD in females may depend on factors other than those determined in this study, in addition to the functional spread of the vascular beds in peripheral tissues, including striated muscle; it is known that the size and the vascular bed in this tissue are affected by exercise training and that this results in the elevation of VO₂max and VO₂max/kg body weight.     

Heat output from the hand of men during acclimatization to altitude and cold

Heat output from the hand of 16 healthy subjects, 22–28 years old, was recorded weekly at Delhi and after they were flown to an altitude of 3, 300 m, where they were divided into two equal groups. One group was exposed to hypoxia only and the other to hypoxia and cold. At the end of three weeks, the groups were interchanged and studied for a further period of three weeks. Thereafter, they were flown back to sea level and retested. There was a significant reduction (p <0.01) in heat output on superimposition of cold stress either in the initial or later phase of acclimatization to altitude, while no significant changes were observed in the absence of cold stress. It appears that local cold acclimatization is inhibited or prolonged at altitude and therefore heat output from the hand cannot be used as an indicator to judge the process of cold acclimatization at altitude.

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Zusammenfassung Die Wärmeabgabe der Hand von 16 gesunden Männern im Alter von 22–28 Jahren wurde im Tiefland (Delhi) und während 6 Wochen Aufenthalt in 3.300 m Höhe untersucht. In der Höhe wurden die Personen in 2 Gruppen aufgeteilt, von denen eine ohne und eine mit Kälteexponierung lebte. Nach 3 Wochen wurden die Bedingungen der Gruppen gewechselt. Nach 6 Wochen erfolgte eine Nachuntersuchung im Tiefland. In der Höhe bewirkte die zusätzliche Kältebelastung in der anfänglichen oder späteren Akklimatisationsphase eine signifikante Verminderung der Wärmeabgabe. Dagegen fehlten diese Veränderungen bei den Personen ohne Kältebelastung. Die lokale Kälteakklimatisation scheint in der Höhe gehemmt oder verlängert zu sein. Deshalb kann die Wärmeabgabe des Vorderarmes nicht als Indikator zur Beurteilung des Vorganges der Kälteakklimatisation in der Höhe geeignet zu sein.

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Resume On a mesuré les pertes de chaleur de la main de 16 hommes en bonne santé dont l'âge était compris entre 22 et 28 ans. Ces mesures furent effectuées en plaine (Delhi) et durant un séjour de 6 semaines à 3300 m d'altitude. En altitude, on a formé 2 groupes dont l'un a été exposé au froid et l'autre pas. Après 3 semaines, les conditions de vie ont été interverties. Après 6 semaines de séjour en montagne, on a effectué un contrôle en plaine. En montagne, la contrainte supplémentaire de l'exposition au froid a eu pour conséquence une réduction de la perte de chaleur aussi bien durant la période précoce que subséquente d'acclimatation. Cette modification n'a au contraire pas été notées chez les personnes non soumises à la contrainte de froid. L'acclimatation au froid semble inhibitée ou au moins ralentie par l'altitude. Pour cette raison, les pertes de chaleur de la main et de l'avant-bras ne sauraient servir d'indicateur dans l'estimation des processus d'acclimatation au froid en altitude.

     

Responses of the autonomic nervous system in altitude adapted and high altitude pulmonary oedema subjects

Studies were carried out to ascertain the role of sympatho-parasympathetic responses in the process of adaptation to altitude. The assessment of status of autonomic balance was carried out in a group of 20 young male subjects by recording their resting heart rate, blood pressure, oral temperature, mean skin temperature, extremity temperatures, pupillary diameter, cold pressor response, oxygen consumption, cardioacceleration during orthostasis and urinary excretion of catecholamines; in a thermoneutral laboratory. The same parameters were repeated on day 3 and at weekly intervals for a period of 3 weeks, after exposing them to 3,500 m; and also after return to sea level. At altitude, similar studies were carried out in a group of 10 acclimatized lowlanders, 10 high altitude natives and 6 patients who had recently recovered from high altitude pulmonary oedema. In another phase, similar studies were done in two groups of subjects, one representing 15 subjects who had stayed at altitude (3,500–4,000 m) without any ill effects and the other comprising of 10 subjects who had either suffered from high altitude pulmonary oedema (HAPO) or acute mountain sickness (AMS). The results revealed sympathetic overactivity on acute induction to altitude which showed gradual recovery on prolonged stay, the high altitude natives had preponderance to parasympathetic system. Sympathetic preponderance may not be an essential etiological factor for the causation of maladaptation syndromes.     

Genetic,acclimatizational and anthropometric factors in hand cooling among North and South Chinese

The left hands of unacclimatized North Chinese (N = 16) and South Chinese (N = 13) were exposed to 5°C water for 30 minutes followed by a 10 minute recovery period. Significant differences independent of body composition were found between the two samples on mean 30 minute temperature during immersion, time and temperature of the onset of initial CIVD (cold-induced vasodilation) at 0.01, 0.05 and 0.10 levels respectively. The result suggests the presence of a genetic component in the cold responses of Continental Asian populations and the possibility of the presence of a clinal distribution of cold response in Asia.     

Changes in cold tolerance due to a 14-day stay in the Canadian Arctic

Responses to cold exposure tests both locally and of the whole body were examined in subjects who stayed in the Arctic (average maximum and minimum temperatures –11 and –21° C respectively) for 14 days of skiing and sleeping in tents. These changes were compared to responses in subjects living working in Ottawa, Canada (average max. and min. temperatures –5 and –11° C respectively). The tests were done before the stay in the Arctic (Pre), immediately after the return (Post 1) and approximately 32 days after the return (Post 2). For the whole-body cold exposure each subject, wearing only shorts and lying on a rope mesh cot, was exposed to an ambient temperature of 10° C. There was no consistent response in the changes of metabolic or body temperature to this exposure in either of groups and, in addition, the changes over time were variable. Cold induced vasodilatation (CIVD) was determined by measuring temperature changes in the middle finger of the nondominant hand upon immersion in ice water for 30 min. CIVD was depressed after the Arctic exposure whilst during the Post 2 testing, although variable, did not return to the Pre values; the responses of the control group were similar. These results indicate that normal seasonal changes may be as important in adaptation as a stay in the Arctic. Caution is advised in the separation of seasonal effects when examining the changes in adaptation after exposure to a cold environment.     

Insulin secretion at high altitude in man

The effect of hypoxia on circulatory levels of insulin, its response to oral glucose administration (100 g) and changes in circadian rhythms of glucose as well as insulin were evaluated in euglycemic males at sea level (SL, 220 m) during their stay at high altitude (3500 m, SJ) and in high altitude natives (HAN).Basal glucose levels were not altered at high altitude but the rise in glucose ( glucose) after glucose load was significantly higher in SJ and HAN (p<0.01) as compared to SL values. An increase (p<0.01) both in basal as well as glucose induced rise in insulin secretion ( insulin) was observed at HA. The rise in insulin in SJ was significantly higher (p<0.01) than in HAN. This elevation in glucose and insulin levels was also evident at different times of the day. The circadian rhythmicity of glucose as well as insulin was altered by the altitude stress. The findings of the study show a rise in insulin level at HA but the hyperglycemia in the face of hyper-insulinism require the presumption of a simultaneous and dispropotionate rise of insulin antagonistic hormones upsetting the effect of insulin on glucose metabolism.Presented at International Conference of Biometeorology held at New Delhi from December 26–30, 1983.     

A new mathematical model to simulate AVA cold-induced vasodilation reaction to local cooling

The purpose of this work was to integrate a new mathematical model with a bioheat model, based on physiology and first principles, to predict thermoregulatory arterio-venous anastomoses (AVA) and cold-induced vasodilation (CIVD) reaction to local cooling. The transient energy balance equations of body segments constrained by thermoregulatory controls were solved numerically to predict segmental core and skin temperatures, and arterial blood flow for given metabolic rate and environmental conditions. Two similar AVA–CIVD mechanisms were incorporated. The first was activated during drop in local skin temperature (<32 °C). The second mechanism was activated at a minimum finger skin temperature, T _{CIVD, min}, where the AVA flow is dilated and constricted once the skin temperature reached a maximum value. The value of T _CIVD,min was determined empirically from values reported in literature for hand immersions in cold fluid. When compared with published data, the model predicted accurately the onset time of CIVD at 25 min and T _CIVD,min at 10 °C for hand exposure to still air at 0 °C. Good agreement was also obtained between predicted finger skin temperature and experimentally published values for repeated immersion in cold water at environmental conditions of 30, 25, and 20 °C. The CIVD thermal response was found related to core body temperature, finger skin temperature, and initial finger sensible heat loss rate upon exposure to cold fluid. The model captured central and local stimulations of the CIVD and accommodated observed variability reported in literature of onset time of CIVD reaction and T _CIVD,min.     

The effects of indomethacin on cold-induced vasodilation in the cat

1. 1. Cold-induced vasodilatation (CIVD) was assessed from records of foot-pad temperatures of 6 domestic cats during immersion of both hind feet in a 0°C water bath.

2. 2. All experiments were performed following anaesthesia with sodium pentobarbital.

3. 3. Four days after the control recordings, the animals were given indomethacin, 5 mg/kg intravenously, and the CIVD response was examined once again; a third test of the cold response was performed 4 days after the treatment with indomethacin.

4. 4. Phasic increases in foot-pad temperature (CIVD) during immersion were smaller (P < 0.05) and delayed in onset (P < 0.05) in the animals treated with indomethacin at a dose which inhibits cyclo-oxygenase.

5. 5. It is proposed that CIVD involves a balance between central symphathetic vasoconstrictor tone and periodic prostaglandin-induced vasodilatation.

Variation and trade-off in reproductive output of the Andean frog<Emphasis Type="Italic"> Hyla labialis</Emphasis>

I analysed variation in number and size of eggs in association with variation in body size of Hyla labialis females from three altitudinally widely separated populations in the Colombian Andes. Females at 3,500 m were significantly larger and heavier than those at 2,700 m, which in turn were larger and heavier than those at 2,000 m. After accounting for interpopulational differences in body size, clutch size (i.e. number of eggs) and egg size differed significantly between populations, but clutch mass did not. At 3,500 m, large relative clutch mass tended to be associated with larger eggs, whereas at lower altitudes it was associated with relatively larger clutch size. Within each population, females showed a significant trade-off between clutch size and egg size, even though relative clutch mass varied substantially and a clutch rarely used up the carrying capacity of their body cavity. At 3,500 m, comparisons between the early and late breeding season within a year suggested that climate fluctuations may play a role in reproductive-output variation within a population. Laboratory-kept females in a high somatic condition after spawning laid larger clutches in the next breeding event, but the trade-off persisted despite ad libitum food supply. Comparisons between field and laboratory suggest that limits to reproductive output were due to physiological, but not morphological restrictions. Therefore, the trade-off is better explained by energy limitation for egg growth depending on clutch size, than by the body cavity limitation hypothesis.     

Cold-Induced Vasodilation during Single Digit Immersion in 0°C and 8°C Water in Men and Women

The present study compared the thermal responses of the finger to 0 and 8°C water immersion, two commonly used temperatures for cold-induced vasodilation (CIVD) research. On two separate and counterbalanced occasions 15 male and 15 female participants immersed their index finger in 20°C water for 5 min followed by either 0 or 8°C water for 30 min. Skin temperature, cardiovascular and perceptual data were recorded. Secondary analyses were performed between sexes and comparing 0.5, 1 and 4°C CIVD amplitude thresholds. With a 0.5°C threshold, CIVD waves were more prevalent in 8°C (2 (1 – 3) than in 0°C (1.5 (0 – 3)), but the amplitude was lower (4.0 ± 2.3 v 9.2 ± 4.0°C). Mean, minimum and maximum finger temperatures were lower in 0°C during the 30 min immersion, and CIVD onset and peak time occurred later in 0°C. Thermal sensation was lower and pain sensation was higher in 0°C. There were no differences between males and females in any of the physiological or CIVD data with the exception of SBP, which was higher in males. Females reported feeling higher thermal sensations in 8°C and lower pain sensations in 0°C and 8°C compared to males. Fewer CIVD responses were observed when using a 4°C (1 (0 – 3)) threshold to quantify a CIVD wave compared to using a 1°C (2 (0 – 3)) or 0.5°C (2 (0 – 3)) amplitude. In conclusion, both 0 and 8 °C can elicit CIVD but 8°C may be more suitable when looking to optimise the number of CIVD waves while minimising participant discomfort. The CIVD response to water immersion does not appear to be influenced by sex. Researchers should consider the amplitude threshold that was used to determine a CIVD wave when interpreting previous data.     

Physiological characteristics of cold acclimatization in man

Studies were conducted on 15 healthy young soldiers to evaluate the effect of a cold acclimatization schedule on the thermoregulatory and metabolic activity on exposure to acute cold stress. These men were exposed to cold (10C) for 4 h daily wearing only shorts for 21 days, in a cold chamber. They were subjected to a standard cold test at 10 ± 1C the day 1, 6, 11 and 21. The subjects were made to relax in a thermoneutral room (26–28C) for 1 h and their heart rate, blood pressure, oxygen consumption, oral temperature, mean skin temperature, mean body temperature, peripheral temperatures, and shivering activity were recorded. Then they were exposed to 10C and measurements were repeated at 30 min intervals, for 2 h. The cold induced vasodilatation (CIVD), cold pressor response and thermoregulatory efficiency tests were measured initially and at the end of acclimatization schedule. The data show that the procedure resulted in elevated resting metabolism, less fall in body temperature during acute cold stress, reduction in shivering, improvement in CIVD and thermoregulatory efficiency and less rise in BP and HR during cold pressor response. The data suggest the possibility of cold acclimatization in man by repeated exposure to moderately severe cold stress.     

Free and total thyroid hormones in humans at extreme altitude

Alterations in circulatory levels of total T₄ (TT₄), total T₃ (TT₃), free T₄ (FT₄), free T₃ (FT₃), thyrotropin (TSH) and T₃ uptake (T₃U) were studied in male and female sea-level residents (SLR) at sea level, in Armed forces personnel staying at high altitude (3750 m) for prolonged duration (acclimatized lowlanders, ALL) and in high-altitude natives (HAN). Identical studies were also performed on male ALL who trekked to an extreme altitude of 5080 m and stayed at an altitude of more than 6300 m for about 6 months. The total as well as free thyroid hormones were found to be significantly higher in ALL and HAN as compared to SLR values. Both male as well as female HAN had higher levels of thyroid hormones. The rise in hormone levels in different ALL ethnic groups drawn from amongst the southern and northern parts of the country was more or less identical. In both HAN and ALL a decline in FT₃ and FT₄ occurred when these subjects trekked at subzero temperatures to extreme altitude of 5080 m but the levels were found to be higher in ALL who stayed at 6300 m for a prolonged duration. Plasma TSH did not show any appreciable change at lower altitudes but was found to be decreased at extreme altitude. The increase in thyroid hormones at high altitude was not due to an increase in hormone binding proteins, since T₃U was found to be higher at high altitudes. A decline in TSH and hormone binding proteins and an increase in the free moiety of the hormones is indicative of a subtle degree of tissue hyperthyroidism which may be playing an important role in combating the extreme cold and hypoxic environment of high altitudes.     

Effects of exposure to a simulated altitude of 3,500 m on calves and oxen

Nine calves and nine oxen were divided into 6 groups and exposed in a climatised low pressure chamber to the following conditions: 2 weeks at 400 m and 4 weeks at 3,500 m. High altitude produced the following changes: increases in heart rate and pulmonary artery pressure, both these changes being larger in the calves than in the oxen. During 4 weeks continuous exposure to 3,500 m, heart rate declined, whereas pulmonary arterial pressure rose. There were increments in respiratory rate, blood-pH, leucocyte number, rectal temperature, blood lactate and blood pyruvate, but no changes in the lactate/pyruvate ratio. Increases in erythrocyte number, haemoglobin, haematocrit, blood specific gravity and blood viscosity were more pronounced in the oxen than in the calves. Feed intake in all animals tended to be depressed in the first half of the high altitude periode. Water intake showed a fall during the first day at 3,500 m, but recovered thereafter. It is concluded that in response to high altitude the calves activated preferentially the circulatory, the oxen the erythropoetic system.     

Quantification of conservative endurance times in thermally insulated cold-stressed digits.

The estimation of endurance times of the digits exposed to cold weather is performed by an analytical, one-dimensional cylindrical model. Blood perfusion effects are lumped into a volumetric heat-generation term. Cold-induced vasodilatation (CIVD) effects are not included in the present analysis. Endurance times, defined by a drop in cylinder tip temperature to 5 degrees C, were evaluated. Parameters included in this evaluation were 1) environmental temperatures, 2) thermal insulation applied on the cylinder, 3) length of the cylinder, and 4) diameter of the cylinder. It was found that the lower the ambient temperature, the longer the finger, and the smaller its diameter, then the shorter the endurance time for the same thermal insulation. Results of the model were compared with measured data for a subject not exhibiting CIVD response to cold stress. Conformity of results calculated for an adjusted value of the volumetric heat-generation term and measured data was very good, with a maximum deviation of less than 10% at only one particular point in time. This model facilitates the conservative estimation of lower bounds to thermally insulated fingers and toes exposed to cold stress.