Wind Chill*

1948 ◽  
Vol 29 (10) ◽  
pp. 487-493 ◽  
Author(s):  
Arnold Court

The rate of heat removal from the human body by wind and low temperature was termed Wind Chill by Siple and expressed by an empirical formula. This paper discusses the formula critically, pointing out that this measure of the convective heat loss may be less than three-quarters of the total heat lost by the body. Siple's formula is compared with those of others, and the use of the formula is discussed.

1979 ◽  
Vol 57 (11) ◽  
pp. 2256-2263 ◽  
Author(s):  
G. J. Gallivan ◽  
K. Ronald

Measurements were made of the relation between body temperature, respiration, diving pattern, and water temperature using three adult harp seals (Phoca groenlandica). Core temperature, ventilation, gas exchange, and diving pattern were not affected by water temperature ranging from 1.8 to 28.2 °C. The basal metabolic rate of the seals in this study was not significantly different than that predicted for terrestrial mammals of equivalent size. Expired heat loss and convective heat loss from the body accounted for 16% of the heat loss and were independent of water temperature. The remaining 84% of the heat was lost from the flippers which accounted for less than 14% of the surface area. Calculations of the ratio of convective heat transfer coefficients of the blubber layer indicate that internal conduction rather than external convection governed heat loss.


MAUSAM ◽  
2022 ◽  
Vol 46 (1) ◽  
pp. 31-34
Author(s):  
E. KULANDAIVELU ◽  
SARBJIT SINGH

The influence of meteorological parameters like wind and temperature determine the chillness upon the human body. The rate of heat removal from the human body by wind and low temperature was termed as Wind Chill by Siple and Passel (1945). Using the wind chill chart wind chill effects at Maitri, Antarctica during 1990 have been studied and compared with conventional value of monthly mean dry bulb and minimum temperatures. It has been observed that the wind chili temperature was about 15°-25°C lower than the dry bulb temperature when the wind speed exceeds 10 kt.      


Resuscitation ◽  
1994 ◽  
Vol 28 (2) ◽  
pp. S9
Author(s):  
A. Zeiner ◽  
M. Frossard ◽  
M. Mullner ◽  
M. Hirschl ◽  
F. Sterz ◽  
...  

2021 ◽  
pp. 103007
Author(s):  
Qiliang Wang ◽  
Yao Yao ◽  
Mingke Hu ◽  
Jingyu Cao ◽  
Yu Qiu ◽  
...  

Solar Energy ◽  
2018 ◽  
Vol 176 ◽  
pp. 496-505 ◽  
Author(s):  
Muhammad Uzair ◽  
Timothy N. Anderson ◽  
Roy J. Nates

1978 ◽  
Vol 100 (1) ◽  
pp. 7-13 ◽  
Author(s):  
L. A. Kuehn

Convective heat loss is a primary cause of hypothermia in humans undergoing water immersion, particularly for swimmers and divers at relatively shallow depths. Various biophysical models have been advanced to account for body heat loss in water of different temperatures and cold stress, most of which have made use of physiological data obtained with easily applied classical thermometry techniques. Explicit techniques for the determination of body heat loss must involve direct calorimetry or the use of heat flow transducers, techniques which are difficult to apply in realistic simulations of actual cold water exposure. This paper describes these latter two techniques in some detail, concentrating on the accuracy to be attained and the calibration necessitated with each method. Results obtained with each method specific to heat loss determination at surface and both dry and wet hyperbaric exposures are shown, illustrating the types of data that can be attained.


2019 ◽  
Author(s):  
Juan F. Torres ◽  
Farzin Ghanadi ◽  
Maziar Arjomandi ◽  
John Pye

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