EOYAL SOCIETY, 



METEOEOLOaY FOR JANUARY, 



Pbivatb Observatory, Hobart Town. 



1866. 



Bar. 37 feet 

 abv. sea level, 

 cor. & reduced 



Self - register- 

 ing Thermo- 

 meters. 



In. In. 

 29-745 29 641 

 29-776 29-772 

 29 -942 129-832; 



4 29-072 29-915 



5 29-776 29-705,' 



6 29-617 29-398 

 7!29-373 29-2971 

 8 '29 -496 29-412 

 9 29-865 29-714 



10 30-034 29-920 

 1129-922.29-8171 



12 29-972 29-6131 



13 29-448 29-370; 



14 29-894 29-726! 



15 29-959 29-905 



16 29-824 29-778 



17 29 -921; 29-910 



18 29-872 29-801 



19 30-049 30-024 

 20^30-155 30-099 

 21 '30 -222 130 -187 



22 30 -209 30 -151 



23 30- 109 '30 -009 



24 29-953 29-631 



25 29-824 29-691 



26 29-957 29-915 

 27,29-882 29-863 

 28 30-080 29-996 

 29:30-136 30'087 

 30 30 -126 1 29 -963 

 31 1 29 -994 1 29 -852 



125-0 53' 

 109-0 52- 

 105-0 49- 

 93-0;40' 

 89-0,50- 

 112-0 56 



Wind. 



d'^ ..: 



■Sif 



figS 



o 



114-0 

 108-0 



89-0 

 110-0 

 116 

 114-0 

 110-0 

 113-5 

 109.0 

 120-0 



81-5 

 104-0 

 103-0 



97-5 

 108-0 



69-0 

 112-0 53 

 123-0 49 

 111-5 56 

 107-0 46 

 106-052 



79-0 '54 

 107-0 55 

 113-0 50 

 115-0150 



NW SE 

 WNW W 



NW SW 



XW W SE 



NW SE 



S SE 



NW W 



NW W 



NW SW 



NW W SE 



10 



NNWS 



NWSE S 



NW W 



NW 



S SE 



E NE SE 



NE SE S 



NW SE 



SW W 



E SE 



SE 



SE E 



NESE 



NW SE 



NW SW 



SW SE S 



NE SE E 



NWSESW 



NW SE 



NW SE 



NW SE S 



.30 



64 



•38 '0-02 



■04 



■26 

 78 

 •33 

 •41 



•78 



•04 



78 



•30 



•46 



•46 



•78 



•04 



.52 



•86 0-01 



-72 1 



•78 



•30 0-03 



•26 0-06 



-52 



•04 



•72 



•52 



•52 



-86 



-86 



•78 



-38 



Mean 29-856, 63-47 105-6 51'74. Total force 75 ^42 0-12 



The mean in all cases is taken from the sums 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 velocity during the month is a very arbitrary one, and 

 the results can be considered only approximately correct. 



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

 are registered each evening at sundown. 



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

 the average. 



