79 



METEOEOLOGY FOR AUGUST, 1866. 



Private Observatory, Hobart Town. 



Bar. 37 feet 

 abv. sea level, 

 cor. & reduced 



In. 

 30-084 

 30-119 



Self - register- 

 ing Thermo- 

 meters. 



In. 

 : 30-065 

 29-987 

 ,30-228 30-177 

 30-365 30-330 

 i 30-345 30-278 

 , 30-313 30-291 

 30-510*30-480 

 30-566 30 -475! 66 

 J 30-492 30 -417 i 65 

 10 30-397 30-234 66 

 ll!30-100 30-018 62 



12 29-992 29 -821 1 66 



13 29-491 29 .385 1 62 



14 29 -785 ,29 -648, 58 



15 29-985 29-942 60 



16 29-719 29-683157 

 17|30-060'29 -911(54 

 18 30 -172! 30- 135 1 62 

 1930-169 .30-129 62 

 20 29-961129-82161 

 2l|29-806 29-567 66 



22 29 -454 '29 -410 62 



23 29-749 29-716 64 



24 30-006,29-853 61 



25 30-082 



26 29.632 

 27129-376 

 28 129-343 

 29 1 29 -448 

 30I29-5OO 

 31 129-792 



29-934 59 

 29-435 56 

 29-245:61 

 29-264 57 

 29-364 55 

 29-444 52 

 29-699(52 



Wind. 



• >5 (D 0) 



(D S .2 



2-5 



41-0 



34-0 



31-5 



31-5 



33-0 



36-0 



40-0 



34-5 



37-5 



35-5 



O'40-O 



034-5 



043-5 



37-0 



Oi28-5 



•0 32-5 



033-0 



0'32-5 



34-0 



039-0 



037-5 



38-0 



36-0 



40-0 



027-5 



036-5 



O'37-O 



■0 38-0 







■0 



•5 



40-0 

 37-5 

 34-5 



NE NW SW 



NWSW 



NWSW 



NW SE 



NW NE S 



NW N S 



NW SE 



NW N 



NWSW 



NW W 



NWSW 



NE NW 



S WNW 



SW S SW 



E N NW 



NW 



SW s 



NW N SE 



NW SE 



NW 



N 



NWW 



W SE NW 



NWSW 



NW SE S 



NW WNW 



N NW N 



N NW 



W SW NW 



NW 



NW SE 



Pi 



il 



0-04 



3-121 



•52 



•261 



•52 

 0- 



•26 



•26' 



•52 



•26 



•78 



•52 

 1-04 

 5-20 0-06 



0-01 



003 



•52 



•26 



•52 



-.52 



•78 



•26 



•52 



•78 



•52 



•52 



5-72 



•26 



3-38 



1.04 



3-64 



5-72 



1.30 



•78 



1-10 

 0-05 



0-20 



0-03 



06 



0-02 

 0-05 

 0-05 

 0-38 

 0-13 

 0-02 



Total force 40 •301bs 1-23 



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 yeais' standard tablei are used for obtaining the differenc* from 

 the average. 



