FREE BOOKS

Author's List




PREV.   NEXT  
|<   22   23   24   25   26   27   28   29   30   31   32   33   34   35   36   37   38   39   40   41   42   43   44   45   46  
47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62   63   64   65   66   67   68   69   70   71   >>   >|  
r does anything more than give nature a better chance, may speedily or more tardily need the service of an undertaker; and the invalid whose powers are responsive to kindly influences may live so long, being unable to get away, that life will be a burden to him. The person in ordinary health will find very little that is hostile to the orderly organic processes. In order to appreciate the winter climate of Southern California one should stay here the year through, and select the days that suit his idea of winter from any of the months. From the fact that the greatest humidity is in the summer and the least in the winter months, he may wear an overcoat in July in a temperature, according to the thermometer, which in January would render the overcoat unnecessary. It is dampness that causes both cold and heat to be most felt. The lowest temperatures, in Southern California generally, are caused only by the extreme dryness of the air; in the long nights of December and January there is a more rapid and longer continued radiation of heat. It must be a dry and clear night that will send the temperature down to thirty-four degrees. But the effect of the sun upon this air is instantaneous, and the cold morning is followed at once by a warm forenoon; the difference between the average heat of July and the average cold of January, measured by the thermometer, is not great in the valleys, foot-hills, and on the coast. Five points give this result of average for January and July respectively: Santa Barbara, 52 deg., 66 deg.; San Bernardino, 51 deg., 70 deg.; Pomona, 52 deg., 68 deg.; Los Angeles, 52 deg., 67 deg.; San Diego, 53 deg., 66 deg.. The day in the winter months is warmer in the interior and the nights are cooler than on the coast, as shown by the following figures for January: 7 A.M., Los Angeles, 46.5 deg.; San Diego, 47.5 deg.; 3 P.M., Los Angeles, 65.2 deg.; San Diego, 60.9 deg.. In the summer the difference is greater. In June I saw the thermometer reach 103 deg. in Los Angeles when it was only 79 deg. in San Diego. But I have seen the weather unendurable in New York with a temperature of 85 deg., while this dry heat of 103 deg. was not oppressive. The extraordinary equanimity of the coast climate (certainly the driest marine climate in my experience) will be evident from the average mean for each month, from records of sixteen years, ending in 1877, taken at San Diego, giving each month in order, beginning with January:
PREV.   NEXT  
|<   22   23   24   25   26   27   28   29   30   31   32   33   34   35   36   37   38   39   40   41   42   43   44   45   46  
47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62   63   64   65   66   67   68   69   70   71   >>   >|  



Top keywords:

January

 

average

 

winter

 

Angeles

 
months
 

temperature

 

climate

 

thermometer

 

California

 

overcoat


Southern

 

summer

 

difference

 
nights
 
warmer
 
Barbara
 

valleys

 

measured

 

forenoon

 

Bernardino


points

 

result

 

Pomona

 
equanimity
 

extraordinary

 

driest

 
marine
 
oppressive
 

unendurable

 
experience

giving
 

beginning

 
ending
 

evident

 
records
 

sixteen

 

weather

 
figures
 

cooler

 

greater


interior

 
health
 

ordinary

 

person

 
burden
 

hostile

 

orderly

 

select

 
organic
 

processes