Tlie Mettorological form brought into ui 

 1870 differs in some respects from the 

 «n adiipted with the view of assimilatir 

 cords more closely with those of s 

 merica, etc., in order to co-operate in 

 ktional Meteorology. Pleadings are add 

 -»de thermometer, that being the instru: 

 1 the continent of Europe. 

 The mean is in all cases taken from tl 

 illy registers, not from the maximum an 

 The direction of the wind is registered 

 iight of 92 feet above sea level, and i 

 ,nare foot. 



The relative quantity of rain that fell 

 Inds i.^ registered each morning at 7 30 i 

 The thirty-five years' standard tables a 

 .e difference from average. 



FKAXCIS ABBO' 



me of leafing, flowering, and fmitinf 

 planta in the Royal Society's Gardt 

 1876 :- 



