ROYAL SOCIETY. 



METEOROLOGY FOR FEBRUARY, 1865. 



Private Observatory, Hobart Town. 



Bar. 37 feet 

 abv. sea level, 

 cor, & reduced 



w 



In., 



1 29 -941 



2 29-82^ 





In. 



29-910 

 29-574 



Self - register- 

 ing Thermo- 

 meters. 



3 29-22^ 29-099 



4 29-57? 29-451 

 29-72^29-706 

 29 70"*i 29-322 



29-507 1 29 -290 

 29 -958; 29 -758 

 29-960,29-818 

 30-132 30-067 

 30- 295 ISO- 289 

 30-258 30-140 

 30 -129 1 30 -086 

 30-063;29-889 

 29-707 29-644 

 29-633 29-556 

 29-635 

 29-844 

 29-892 

 30-093 

 29-955 

 29-686 

 29-755 

 29-702 

 29-756 

 29-908 

 29-443 

 29-567 



29-774 

 29-871 

 29-971 

 30-132 

 30-069 

 29-912 

 29-762 

 29-710 

 29-857 

 29 954 

 29-724 

 29-849 



Wind. 



1^ ^ 



100-0 41-0 NWSES 

 104-0 56 -OjNE SE SE 



78-0 49-USWNWSW 

 100-0 40-0 SW NW 

 114-0 42-0 NW 

 110-0 51-0 NW N 



88-0 46-0 NWNE N 

 lOl-o 39-0 NEW NW 

 109-045-5' NW W 

 118-0,46-0 NSW NW 

 113-0^44-0 NW SE S 

 122-0l50 5 NW N SE 

 120-0 50-51 SE 

 120-0 53-0 W SE E 



90-0'58-0NENWSE 



112-0,50.0 



89-0 49-0 



103-0 45-0 



NS W W 

 NW SE 



N SE 



92-0 45-5 SE NE SW 

 lll-0;52-0l N SE S 

 118-046-0| N Sbl 

 53 120 50-0; N NW SE 

 56' 115-0 -530 SWSESW 



56 107-0 51-0 

 55l 97-0:50-0 



108-0 44 

 110-5 54-0 

 114-0 51-0 



NW W 

 NWNW 



NWSESW 



NNWN 

 NNW 



52 0-06 



■78 0.67 

 2.60 0-02 

 8-33 



•520-19 

 5-20 . 

 1-0410*15 

 3 -12 1 0-05 

 l-04|0-73 



•78 

 1-04 



•78 



.20 



•26 

 1^04 



-78 



•52 



•78 

 0- 



'78 



-.52 

 1-04 

 1-04 

 1-04 

 1-30 

 3.12 



•52 

 5^46 



0-03 

 0-02 

 0-90 

 0-19 

 0-10 



0-02 



0-24 

 0-22 



I Total force 44 -211b3. 



The mean in all cases is taken from the sums of the three daily registers, 

 and not from the maximum and mir imum. 



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

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

 however, of an uniform velocity during the mouth is a very arbitrary one, and 

 the results can be considered only ajiproximately correct. 



The relations of the quantities of rain which fell under the different winds, 

 are registered each evening at sun-down. 



The twenty years' standard tables arc used for obtaining the difference from 

 the average. 



B 



