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University of Wollongong
Research Online
Faculty of Health and Behavioural Sciences - Papers Faculty of Health and Behavioural Sciences
2009
e roles of hands and feet in temperature
regulation in hot and cold environments
Nigel A.S. Taylor
University of Wollongong, nigel_taylor@uow.edu.au
Christiano Machado-Moreira
University of Wollongong, cam313@uow.edu.au
Anne van den Heuvel
University of Wollongong, amjvd453@uow.edu.au
Joanne Caldwell
University of Wollongong, jnc063@uow.edu.au
Elizabeth A. Taylor
University of Wollongong
See next page for additional authors
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Publication Details
Taylor, N. A.S.., Machado-Moreira, C., van den Heuvel, A., Caldwell, J., Taylor, E. A.. & Tipton, M. J.. e roles of hands and feet in
temperature regulation in hot and cold environments. irteenth International Conference on Environmental Ergonomics; Boston,
USA: University of Wollongong; 2009. 405-409.
e roles of hands and feet in temperature regulation in hot and cold
environments
Abstract
In this paper, we briey review the physiological and biophysical characteristics of the hands and feet, and
their association with autonomic (physiological) and behavioural temperature regulation, and with thermal
injury. A comprehensive review of this topic is not currently available within the literature. e temperatures
of the skin and subcutaneous tissues, particularly those of the hands and feet, vary signicantly as air
temperatures move away from the thermal comfort zone. Mean skin temperature increases approximately
0.7oC for each 1oC elevation in air temperature, with smaller changes at the hands (0.46o.oC-1) and slightly
larger changes at the feet (0.8o.oC-1: Bedford, 1936). ese variations reect local dierences in metabolic
rate, convective heat delivery (mass ow) and thermal exchanges with the thermal environment.
Keywords
hot, hands, cold, environments, feet, temperature, regulation, roles
Publication Details
Taylor, N. A.S.., Machado-Moreira, C., van den Heuvel, A., Caldwell, J., Taylor, E. A.. & Tipton, M. J.. e roles
of hands and feet in temperature regulation in hot and cold environments. irteenth International
Conference on Environmental Ergonomics; Boston, USA: University of Wollongong; 2009. 405-409.
Authors
Nigel A.S. Taylor, Christiano Machado-Moreira, Anne van den Heuvel, Joanne Caldwell, Elizabeth A. Taylor,
and Michael J. Tipton
is conference paper is available at Research Online: hp://ro.uow.edu.au/hbspapers/190
Proceedings of the 13th International Conference on Environmental Ergonomics, Boston (USA), August 2-7, 2009
405
THE ROLES OF HANDS AND FEET IN TEMPERATURE REGULATION
IN HOT AND COLD ENVIRONMENTS.
Nigel A.S. Taylor1, Christiano A. Machado-Moreira1, Anne M.J. van den Heuvel1,
Joanne N. Caldwell1, Elizabeth A. Taylor1 and Michael J. Tipton2
1Thermal Physiology Laboratory, University of Wollongong, Wollongong, Australia
2Human and Applied Physiology Laboratory, University of Portsmouth, Portsmouth, England
Contact person: nigel_taylor@uow.edu.au
INTRODUCTION
In this paper, we briefly review the physiological and biophysical characteristics of the hands
and feet, and their association with autonomic (physiological) and behavioural temperature
regulation, and with thermal injury. A comprehensive review of this topic is not currently
available within the literature.
The temperatures of the skin and subcutaneous tissues, particularly those of the hands and feet,
vary significantly as air temperatures move away from the thermal comfort zone. Mean skin
temperature increases approximately 0.7oC for each 1oC elevation in air temperature, with
smaller changes at the hands (0.46o.oC-1) and slightly larger changes at the feet (0.8o.oC-1:
Bedford, 1936). These variations reflect local differences in metabolic rate, convective heat
delivery (mass flow) and thermal exchanges with the thermal environment.
NEURAL PATHWAYS
Thermoregulation is achieved by modulating physiological efferent functions (skin blood flow,
sweating, shivering) and implementing behavioural strategies, following the central integration
of thermal feedback from the deep body and superficial tissues. In all environments, cutaneous
thermoreceptors provide the first thermal feedback signals, giving rise to thermal sensations,
physiological adjustments and eventually to decisions relating to the pleasantness or comfort that
the environment and associated responses evoke.
The principal nerves carrying thermoreceptor feedback from the hand are the radial and median
nerves, with the latter having a more important sensory role. This feedback travels to the spinal
cord via the 6th, 7th and 8th cervical spinal nerves, and eventually to the hypothalamus. For the
foot, the corresponding nerves are the tibial, sural and superficial fibular nerves, which enter the
spinal cord via the 1st sacral and 5th lumbar spinal nerves: these nerves also relay efferent signals
that control blood flow, sweating and muscular function. The nerves that dictate thermoeffector
function of the hand leave the spinal cord at the thoracic segments (T2-T8), while those for the
foot leave at the thoracic and lumbar segments (T11-L2).
Most neurones of the sympathetic nervous system are noradrenergic. However, this does not
hold for the thermoefferent fibres, which possess at least three different neurotransmitters. For
instance, the fibres that innervate most eccrine sweat glands are cholinergic, with perhaps some
evidence of noradrenergic control at the glabrous (hairless) surfaces of the hands and feet. Skin
blood flow to these glabrous surfaces is determined solely by noradrenergically mediated
vasoconstrictor nerves (Kellogg, 2006). In contrast, blood flow to the non-glabrous (hairy) skin
regions is mediated by separate noradrenergic vasoconstrictor and active vasodilatory branches
Proceedings of the 13th International Conference on Environmental Ergonomics, Boston (USA), August 2-7, 2009
406
of the sympathetic nervous system; the neurotransmitter for the latter pathway awaits
identification (Kellogg, 2006).
VASCULAR FUNCTION AND DYSFUNCTION
Blood flow to the hands is provided through the radial and ulnar arteries, and via the deep palmar
arch, the superficial palmar branch, the metacarpal arteries and the digital arteries. In the foot,
blood enters from behind each of the malleoli (malleolar arteries) and across the upper surface of
the foot (dorsalis pedis artery). The positioning of these vessels with respect to the bones of the
foot has significant implications for shoe design. Cutaneous capillaries are located just below the
epidermis, with hand veins draining into either superficial or deep vessels, the largest of which
run along the dorsal hand and foot surfaces. Hands and feet also contain arteriovenous
anastomoses, and when these shunts are open, dramatic elevations in skin blood flow can occur.
Indeed, these vessels are responsible for the extremities behaving as very efficient heat
exchangers (radiators), with thermal homeostasis sometimes being achieved entirely through
subtle changes in skin blood flow through the anastomoses of the hands, face and feet (Hales,
1985).
Under thermoneutral conditions, hand blood flow (10 mL.100 mL-1.min-1; Roddie, 1983) is
typically 3-4 times greater than that of the foot (3 mL.100 mL-1.min-1; Colemont and Decoutere,
1981). When normalised to the skin surface area, hand blood flow is 4-5 times greater than the
rest of the body, and about twice that of the foot (Taylor et al., 2008a). During protracted cold
exposures, extremely low local blood flows are observed (hand: 0.15 mL.100 mL-1.min-1; foot:
0.2 mL.100 mL-1.min-1; Taylor et al., 2008a, b), and such flows can be below the metabolic
requirements of these tissues. In the heat, maximal hand blood flow approximates 30 mL.100
mL-1.min-1, while 18 mL.100 mL-1.min-1 appears maximal for the foot (Taylor et al., 2008a, b).
Finger blood flows have greater minimal (0.2 mL.100 mL-1.min-1) to maximal variations (120
mL.100 mL-1.min-1) with changes in whole-body thermal state (Nagasaka et al., 1987). In
addition, blood flow at the middle phalanx is only about 30% of that at the distal phalanx
(Wilkins et al., 1938).
The single most important determinant of hand and foot blood flow is the thermal status of the
body core (Ferris et al., 1947), with a 1oC change in mean skin temperature producing a 1.3 fold
change (10 mL.100 mL-1.min-1) in finger blood flow, and the corresponding change in core
temperature resulting in a 2.8-fold change (32 mL.100 mL-1.min-1; Wenger et al., 1975). Thus,
local temperatures can influence blood flow, but this affect is minimal when the body core is
either hot or cold, and it is greatest when deep body temperature is within the thermoneutral
range.
The blood supply to the hands and feet represents their primary source of heat, and the minimal
blood flows seen with deep and superficial tissue cooling, as a result of intense peripheral
vasoconstriction, represent a physiological amputation of these appendages. The consequence of
this is a loss of both sensation and function, and in particular manual dexterity. Insufficient tissue
perfusion and heat loss affect vascular smooth muscle contractility, which can, if core
temperature is normal or raised, result in vasodilatation. This cold-induced vasodilatation can
protect tissues from, and delay tissue damage. In the absence of tissue warming, extreme or
prolonged cooling of the extremities can result in non-freezing and freezing cold injury. The
Proceedings of the 13th International Conference on Environmental Ergonomics, Boston (USA), August 2-7, 2009
407
former condition has recently been associated with a cold-induced defect in vascular smooth
muscle contractility caused by a loss of NO-dependent endothelial function (Stephens et al.,
2009).
BIOPHYSICAL ATTRIBUTES
Relative to the entire body, the surface area to mass ratio for the hand is 4-5 larger, while that for
a foot is 2.5-3 larger (males-females). Therefore, these appendages provide an effective route for
heat exchange with the environment, as long as thermal energy can be delivered from the body
core via convective (mass flow) pathways.
The maximal hand and foot blood flows (30 and 18 mL.100 mL-1.min-1) can result in theoretical
peak heat transfers from the core to both hands of 12 W or 286 W.m-2 for a 1oC core-skin
gradient. The corresponding values for both feet are 16 W or 404 W.m-2. Thus, while the
absolute heat transfer to the hands and feet from the body core is not high, their surface-area
normalised transfer, when considered in combination with the huge capacity of the arteriovenous
anastomoses to elevate local skin blood flow, makes these appendages very important locations
for heat dissipation (Taylor et al., 2008a; 2008b).
This heat delivery, and its subsequent dissipation, is advantageous in the heat, as it facilitates
central cooling, but, as described above, it can be dangerous in the cold. Furthermore, these data
also represent maximal core-periphery transfers, and not that which occurs between the skin and
its surrounding environment. By using foot and hand temperatures observed during actual air
exposures to 15o, 27o and 45oC (Webb, 1992), the theoretical radiative and convective heat
transfers from each hand and foot to the surrounding air may be computed, and these represent
respective losses of 16.6 W and 25.5 W (15oC), and 7.7 W and 11.8 W (27oC), or gains of 18.1
W and 27.7 W (45oC). More impressive heat transfer occurs when the vasodilated appendages of
heated individuals are placed into cold water (Tipton et al., 1993). In this circumstance, heat loss
can range from 70-85 W (hands) and 90-95 W (feet: House and Tipton, 2002).
SUDOMOTOR FUNCTION
Sweat glands are widely distributed over the body surface, with a total of two-four million glands
capable of producing sweat at peak rates of 10-15 L.d-1. Each hand has approximately 160,000
eccrine sweat glands, with greater numbers on the palmar (115,000) than dorsal surface (46,000:
Machado-Moreira et al., 2008). Similarly, one foot has approximately 155,000 glands, with more
on the plantar (100,000) than the dorsal surface (55,000; Taylor et al., 2006).
Both the hands and feet display two general sweat patterns during heating: low secretion at the
glabrous surfaces, and moderate secretion from all other surfaces. During passive heating at rest
(40 min), where the average whole-body skin temperature was increased from 34.5oC to 35.9oC,
and core temperature was elevated to 37.2oC from 36.9oC, the palms and soles displayed the
lowest intra-segmental sweat rates (palm: 0.16 mg.cm-2.min-1; sole: 0.23 mg.cm-2.min-1).
Conversely, the dorsal surfaces of the distal phalanges of the fingers (0.62 mg.cm-2.min-1) and
the distal phalanx of the big toe (0.50 mg.cm-2.min-1) displayed the highest sweat rates. Under
these experimental conditions, sweating averaged 0.38 mg.cm-2.min-1 from the hands (Machado-
Moreira et al., 2008) and 0.45 mg.cm-2.min-1 from the feet (Taylor et al., 2006).
Proceedings of the 13th International Conference on Environmental Ergonomics, Boston (USA), August 2-7, 2009
408
When exercising in the heat, sweat gland recruitment occurs almost simultaneously across most
body surfaces, including the hands and feet, although the intra-segmental distribution is not
uniform. The dorsal surfaces of both appendages display a relatively consistent secretion rate,
accounting for approximately 65-70% of total sweat flow from each extremity. Peak hand sweat
rates during heavy exercise are: 4.0 mL.h-1 (palm); 16.8 mL.h-1 (volar fingers); 16.6 mL.h-1
(dorsal fingers); and 15.0 mL.h-1 (dorsal hand: Machado-Moreira et al., 2008). Corresponding
sweat production from the foot is: 14.5 mL.h-1 (dorsal), 5.4 mL.h-1 (medial) 5.0 mL.h-1 (lateral),
16.0 mL.h-1 (plantar), 2.9 mL.h-1 (dorsal toes), and 1.1 mL.h-1 (plantar toes; Taylor et al., 2006).
Therefore, the maximal theoretical evaporative cooling possible from a single hand is about 35.4
W (assuming 100% evaporation), and 27.6 W from one foot. Indeed, when normalised to surface
area, the potential for evaporative heat loss from the two hands is 110% greater than at the torso,
and 200% greater than at both feet, but only half that of the forehead (Taylor et al., 2008b).
THERMAL SENSATION AND DISCOMFORT
Thermal sensations arise within the somatosensory cortex. Sensory feedback from the face and
hands, and to a lesser extent the feet and toes, is very powerful as these areas provide feedback to
a larger volume of the somatosensory cortex (Penfield and Rasmussen, 1952). Discomfort drives
behaviour, based upon the pleasantness of a given thermal state, and while this sensation is
related to both the core and peripheral temperatures, it is believed that thermal comfort is
primarily determined by the thermal state of the core (Hensel, 1981). It is known that a
separation exists between local and whole-body discomfort, such that one can have
uncomfortable feet while the rest of body remains thermally comfortable. However, the face,
hands and feet are associated with significantly greater thermal discomfort with local tissue
temperature changes. Indeed, the hands and feet provide very powerful feedback relative to local
comfort, but play a minimal role relative to whole-body thermal discomfort (Cotter et al., 1996).
These high local sensitivities are important to clothing design, but are of less importance to
behavioural responses. The head, however, dominates whole-body thermal sensation and
discomfort (Cotter and Taylor, 2005), so the thermal status of the face has a more powerful role
in dictating thermoregulatory behaviour.
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ACKNOWLEDGEMENT
Some of the research reported within this review was supported by grants from W.L. Gore &
Associates GmbH (Germany) and from the Ministry of Defence (Republic of Slovenia).