126 DETERMINATION OF ALTITUDES BY BAROMETER. 



Whenever water-courses gave practical checks upon the relative altitudes of different stations, 

 as was often the case, the profile bore the most careful study in a perfectly satisfactory manner, 

 and confirmed, without exception, the use of the mean daily air temperature, instead of the 

 observed, in the computation. 



HEIGHT OF FORT HEADING; EXPLANATION OF TABLES OF BAROMETRIC OBSERVATIONS, ETC., IN 



APPENDIX D. 



The great number of observations taken at Fort Reading bas enabled me to compute its alti 

 tude in two different ways ; one of which is independent of the tables of horary and abnormal 

 correction. We had very careful hourly observations taken from July 22 to July 26, and from 

 November IT to November 22, inclusive. It is well known that a mean of the observations at 

 7 a. m., 2 p. m., and 9 p. m., differs very little from the mean barometric reading for the 

 whole twenty-four hours ; and, as five of the days on which the above mentioned observations 

 were taken were in the dry, and six in the rainy season, it is probable that a mean of their 

 mean readings thus found may approximate to that of the year. It is 29.500 inches. The 

 corresponding mean air temperature, found by taking a mean of the observations at 7 a. m., 

 12 m., and 10 p. m., for the eleven days, is G2.3 Fall. The altitude given by these data is 

 518 feet. 



By the second method, I applied the tables as in other cases, and found the corrected mean of 

 all our observations at the fort, which were about 600 in number, and, with the corresponding 

 mean air temperature, computed the altitude. It is 544 feet, differing only 26 feet from the 

 other. I have adopted the first result on the profiles, as it is obtained from observations taken 

 with very great care, while many of the others are less reliable. 



The tables in Appendix D exhibit the original data for the construction of our profiles, 

 and the altitudes deduced from the observations. It must be remembered that all the altitudes 

 are referred to the level of mean tide at Benicia, as the barometric reading at the sea level 

 north of that place is not known. The column headed &quot;corrected barometric reading&quot; gives 

 the height of the mercurial column, after the corrections for reduction to 32 Fahr., for instru 

 mental error, and for horary and abnormal oscillation, have been applied. The very slight 

 difference between these corrected readings, when there are several taken at the same camp, 

 confirms the accuracy of the horary and abnormal tables. 



