M 

 Pri 



Latituc 



The Meteorological form broi:ght into u 

 if 1876 differs in some respects from the i 

 •een adopted with the -vdew of assimilatin 

 ecords more closely with those of stations i 

 tc. in order to co-operate in a systei 

 deteorology. Readings are added from t 

 aometer, that being the instrument gen 

 lontineni of Europe. 



The mean is in all cases taken from tl 

 laily registers, not from the maximum and 



The direction of the wind is registered 

 leight of 92 feet above sea level, and i 

 i^uare foot. 



The relative quantity of rain that fell i 

 vinds is registered each morning at 7-30 a. 



