Arizona Sketches by J. A. (Joseph Amasa) Munk
page 124 of 134 (92%)
page 124 of 134 (92%)
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The humidity caused by an abundant rainfall in any low, hot
country is usually enough to unfit it for human habitation. The combined effect of heat and moisture upon a fertile soil causes an excess of both growing and decaying vegetation that fills the atmosphere with noxious vapors and disease producing germs. The sultry air is so oppressive that it is more than physical endurance can bear. The particles of vapor which float in the atmosphere absorb and hold the heat until it becomes like a steaming hot blanket that is death to unacclimated life. All of this is changed where siccity prevails. The rapid evaporation quickly dispels the vapors and the dry heat desiccates the disease creating germs and makes them innocuous. The effect of heat upon the body is measured by the difference in the actual and sensible temperatures, as recorded by the dry and wet bulb thermometers. When both stand nearly together as they are apt to do in a humid atmosphere, the heat becomes insufferable. In the dry climate of Arizona such a condition cannot occur. The difference in the two instruments is always great, often as much as forty degrees. For this reason, a temperature of 118 degrees F. at Yuma is less oppressive than 98 degrees F. is in New York. A low relative humidity gives comfort and freedom from sunstroke even when the thermometer registers the shade temperature in three figures. A dry, warm climate is a stimulant to the cutaneous function. The skin is an important excreting organ that is furnished with a large number of sweat glands which are for the dual purpose of furnishing moisture for cooling the body by evaporation and the elimination of worn out and waste material from the organism. As |
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