Immediately following exercise the muscles are able to replenish glycogen
stores at a much higher level than a few hours later,
| Try a protein-carb mix to more rapidly replenish your glycogen stores after a long run. But don't forget your overall fluid replacement needs should be met with a sports drink or water. |
To help you stay hydrated during this long, hot summer of running you
might consider stopping at every water fountain you pass and taking a drink.
Don't forget to give yourself a few weeks to acclimate to the heat. This
is best done by running 3 to 4 miles
| Try combining treadmill running and outside running to get more distance on the really hot days. |
And now on to the facts.
Heat Production:
During exercise, heat is produced in direct relationship to the amount of energy expended. In running, this results in speed being the primary determinant of body heat production. Elite runners would run at an energy level expenditure of 1500 kcal/hr while a novice runner would be likely to run at an energy level expenditure rate of 500 kcal/hr. Body metabolism as a means of energy production is estimated to be only 25 percent efficient. That leaves 75 percent of the energy used going solely to the production of heat. That is great for cold weather, but not of much help to hot weather runners.
The radiant energy of the sun may be responsible for up to 150 kcal/hr on a clear and cloudless day. Heat production alone would thereby give an average runner a heat burden of approximately 1000 to 1200 kcal/hr. If there were no means of heat dissipation the core temperature would rise by approximately 23 degrees. In other words, if there were no functioning thermoregulation, the body temperature would rise approximately 1 degree centigrade for every 5 to 8 minutes of running.
Heat Loss:
As we have already mentioned, perspiration and evaporation of perspiration, is the primary means for the body to cool during exercise. Skin blood flow increases significantly during exercise. Blood flowing near the surface results in cooling by both conduction and convection. There appears to be a 25 to 40 percent lower increase in Skin Blood Flow, however, in the older athlete. Sweat glands become active as body core temperature rises. One liter of sweat is generated during the expenditure of about 500 kcal. Studies have shown that training increases both sweating and skin blood flow.An individual who is heat acclimated may perspire almost twice as much as an unacclimated individual.
An individual who is heat acclimated may perspire almost twice as much as an unacclimatized individual. One of the effects of acclimatization is to allow an individual to begin perspiration earlier in the course of exercise, this allows for a quick, effective and efficient beginning to heat dissipation and alleviation of early heat buildup. Each gram of perspiration that evaporates cools the body by 0.6 kcal. Acclimatized individuals may produce up to 30 g/minute of perspiration. This would allow for considerable cooling.
As we noted, the environment has a major impact on heat loss. Humidity, playing the largest role, but temperature, of course, also a major factor. These both impact upon heat loss via conduction and convection besides the impact on evaporation of perspiration. The worst possible conditions would be a hot, humid, windless day, following a cool spell.
Treatment should be to get the individual to a cool shaded area and administer fluids either by mouth, if conscious or IV if the individual is unconscious. Seek medical advise.
Heat stroke is caused by a sudden failure of the thermoregulatory system of the body. Heat stroke may be fatal. Some consider it to lie on a continuum with heat exhaustion. It initially appears similar to heat exhaustion, but may rapidly progress to manifest more serious neurological symptoms: disorientation, loss of consciousness and seizures (status epilecticus). The body temperature may be higher than 104 degrees Fahrenheit. Sweating is often absent, but the skin may be quite moist from earlier perspiration. The core temperature must be brought down immediately. In fun runs, perspiration is usually noted, and you do not need the absence of perspiration or an rectal temperature to make the diagnosis. There is usually a sinus tachycardia present, with the pulse noted to be faster than 160. The blood pressure may be low. Kidney damage (acute nephropathy) occurs in about 35 per cent of cases. Rhabdomyolysis (muscle breakdown) occurs and the myoglobulinuria (excretion of muscle breakdown products) contributes to the kidney injury. Liver damage is also evident when liver enzymes are measured following heatstroke.Heat stroke may be fatal
These are the individuals who get "packed in ice". Rapid medical attention is vital.
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DERIVED FROM TEMPERATURE AND RELATIVE HUMIDITY
|
10% 65 70 75 80 85 90 95 100 105 111 116
20% 66 72 77 82 87 93 99 105 112 120 130
30% 67 73 78 84 90 96 104 113 123 135 148
40% 68 74 79 86 93 101 110 123 137 151
50% 69 75 81 88 96 107 120 135 150
60% 70 76 82 90 100 114 132 149
70% 70 77 85 93 106 124 144
80% 71 78 86 97 113 136
90% 71 79 88 102 122
100% 72 80 91 108
At an apparent temperature of:
90-104 Heat cramps or heat exhaustion possible
105-130
Heat cramps or heat exhaustion likely,
heatstroke possible
130-more Heatstroke highly likely
Note: Combined heat index of heat and humidity, what it "feels like"
Exposure to full sunshine can increase
considerably.
In case nothing jumps out at you in this jumble of numbers, let's look at a typical example for Washington, D.C. Let's say you get up a bit late on a Saturday morning, after a Friday night of "renting" beer. A touch dehydrated, but unaware of this, you decide to go out for a run around 11:30 A.M. You head for Rock Creek Park, in the shade. It's hot but what the heck, you planned to run about 7 to 8 miles. Off you go. It's humid, sticky, hot, one to two miles later you feel as if you'd run 5 miles already. You wise up, turn around and have completed between 3 - 4 miles, feel as if you'd done 10 without training. Later you find out the temperature was 102 degrees.With the humidity at greater than 70%, 100 degrees would feel like 144 degrees. When the humidity is 90%, 90 degrees will feel like 113 degrees. Hmmmmm, maybe it is not such a good idea to run then!
WBGT = 0.7 x Twb + 0.2 x Tg + 0.1 xTdb
Twb = Wet bulb temperature
Tg = Black globe temperature
Tdb = Dry globe temperature
From this formula, it is evident that the humidity is valued as the major determinant of heat stress, as it is weighted at 70% of the value. Below a WBGT value of 64 degrees (18 C) the risk of heat injury is small. Above a WBGT value of 82 degrees (28 C) races should not be undertaken.
S= M + R + CD + Cv - ES = stored heat
From this formula it is evident that heat balance in the body depends upon the amount of heat produced by muscle activity and metabolism and the amount of heat that is gained or lost either by the effect of the environment and evaporation of perspiration. Note that perspiration that drips from your body does not appreciably contribute to evaporative heat loss. Air flow either through the effect of wind or your own body motion does aid the cooling of the body. The sudden loss of this air flow is one of the reasons why you will start sweating more when you stop running.
Stay

The heat index formula gives good results for temperatures above 70 degrees Fahrenheit. The formula is as follows: t = temperature in degrees Fahrenheit, r = %relative humidity (-42.379+2.04901523*t+10.14333127*r-.22475541*t*r-(6.83783e-3)*t^2- (5.481717e-2)*r^2+(1.22874e-3)*t^2*r+(8.5282e-4)*t*r^2-(1.99e-6)*t^2*r^2)
This formula was posted to rec.running by Phil Margolies and he reports it is more accurate than the Javascript above.
For the heatedly obssessed Phil Margolies also posted the following
Excel formula:
You can paste the following forumula on an Excel spreadsheet. If you
put the temperature in cell A1 and the relative humidity in cell B1 and
paste this formula in cell C1: =-42.379+2.04901523*(A1)+10.14333127*(B1)-0.22475541*(A1)*(B1)-0.00683783*(A1*A1)-0.05481717*(B1*B1)+0.00122874*(A1*A1)*B1+0.00085282*(A1)*(B1*B1)-0.00000199*(A1*A1)*(B1*B1)