ROYAL SOCIETY. 



METEOROLOaT FOR JAmJARY, 1865. 



Private Observatort, Hobart Town. 



Bar. 37 feet 

 abv. sea level, 

 cor. & reduced 



In. 



1 29-706 



2 29-991 



3 30.175 



4 30-034 

 5129-75.5 

 6 29-882 

 7129-987 



8 29 776 



9 29-801 

 10 29-797 

 Hi 29 -822 

 12. 30 -015 

 13.30-118 



14 30 -160 



15 30-079 



16 29-930 



17 29-604 



18 29-813 



19 29-921 

 20.30-008 

 21129-803 



22 29-660 



23 29-744 



24 29-802 



25 29-779 



26 30-086 

 27]30-129 

 28 29-949 

 29:. 30- 049 

 30|30 0O8 

 31 '29 -839 



In. 



29-679 

 29-845 

 30-1.58 

 29-739 

 29-684 

 29-837 

 29-976 

 29-506 

 29-690 

 29-740 

 29-764 

 29-970 

 30-100 

 30-113 

 29-992 

 29-606 

 29-464 

 29-793 

 29-834 

 29-960 

 29-585 

 29-590 

 29-5.58 

 29-732 

 29-757 

 30-029 



30 -091 ; 



29-846: 

 30-0301 



29-747 

 29-6911 



Self - register- 

 ing Thermo- 

 meters. 



53 



47 

 48 

 76:52 

 72 50 

 74150 

 69 55 

 69 54 



66 49 

 72 48 



72 56 

 67149 



63 50 



64 46 

 7051 



73 46 

 7158 



67 49 



67 52 



68 43 



72 43 

 67 51 

 7155 



69 .50 



70 46 



65 .52 



73 .52 

 76.57 

 72.52 

 78.53 

 65 56 



70 

 105 

 101 

 118 

 110 

 112 



98 



84 

 105 

 115 

 106 

 107 

 107 



89 



50-0 

 43-0 

 47-0 

 49-0 

 53-0 

 49-0 

 50-0 

 50 

 45-0 

 47-0 

 50-5 

 45-0 

 43-0 

 42-0 



kWind. 



11 5148-0 

 122143-0 

 11048-5 

 110:47-0 

 110{49-0 

 112 40-5 

 112 45-5 



81 48-0 



99 51 -0 

 11140-5' 

 100 49 



78 .50 

 110 .50-0 

 11553-0 

 107 .50.0 

 120 48-5 



99,48-0 



.02 

 •02 



•02 



*04 

 •06 



-07 



I Total force 71-79 • [ 

 The mean in all cases is taken from the su-ms of the three daily registers 



and not from the maximum and minimum. 

 The direction of the wind is registered from currents moving at a height of 



192 feet, and the force according to Lind's Wind Guage. The supposition, 



however, of an uniform velocitj'^ during the month is a very arbitrary one, and 



the results can be considered only approximately corrects 



