1. Finger blood flow was estimated, by strain‐gauge plethysmography, before and during a 1 hr immersion in ice water, on twenty‐five men throughout a year at Wilkes, Antarctica. A total of 121 satisfactory immersions were made. 2. Blood flow before and during immersion decreased significantly in the colder months of the year, and the increase caused by cold‐induced vasodilatation (CIVD) became less as the year progressed. The time of onset, blood flow at onset, and frequency of the cycles of CIVD showed no significant relation to the coldness of the weather (as measured by mean monthly wind chill) or the time in months. Comparisons of blood flow before and after five field trips (average duration 42 days), on which cold exposure was more severe than at Wilkes station, gave similar results. 3. The results suggest that vasoconstrictor tone increased. This interpretation agrees with previous work on general acclimatization in Antarctica, but contrasts with work elsewhere on local acclimatization of the hands. © 1968 The Physiological Society
CITATION STYLE
Elkington, E. J. (1968). Finger blood flow in Antarctica. The Journal of Physiology, 199(1), 1–10. https://doi.org/10.1113/jphysiol.1968.sp008636
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