14 



JRelatice Humidity, 



^'^- JDaareeyS of TempentXur», ^JF.) 



atures. The rate of increase forms a curve, as shown in the diagram 



annexed, but increasing in 

 percentage more slowly as 

 the temperature is high. 

 These curves are higher 

 when the wet and dry bulb 

 thermometers are nearer 

 alike, and grow smaller at a 

 regularly decreasing rate as 

 the differences between in- 

 struments increase. 



60. At all temperatures, 

 the relative humidity dimin- 

 ishes in percentage as the 

 difference between the in- 

 struments increases, as we 

 see by the descending curves 

 in Figure 4, but not at uni- 



!?. Eelative Humidity at different Tempera- form rates, as We see that 



these lines arc curves. The 

 degrees marked on these 

 curves from 0° to 100° are 

 those of temperature in the 

 open air.' 



(1) The numerical Etatements 

 frcim which this and the preced- 

 ing figures sue constructed will 

 be found in a volume of meteor- 

 ological tables prepared bj- Pro- 

 fessor Guj-ot, and published by 

 the Smithsonian Institution for 

 the use of its observers, at the 

 time when the former system 

 of voluntary meteorological ob- 

 servation was in operation. The 

 limits of this volume do not ad- 

 mit of their insertion in detail, 

 nc r of a statement of the 



principles upon which thev are 

 4. Relative Humidity at fixed Temperaturesi . , 

 theflifferenoe.betweeuwetand dry Bulbs being bused, 

 variable. 



tures the difference between wet'and dry liulbs 

 being constant. 



