31 



METEOROLOaY FOR APRIL, 1866. 



Private Observatory, Hobart Town. 



Bar. 37 feet 

 abv. sea level, 

 cor. & reduced 



In. 



1 30-106 



2 i 29 -944 



3 29-900 

 4,29-782 

 529-984: 

 6 30-193 



Self ■■ register- 

 ing Thermo- 

 meters. 



76 56 



71 



30-227 

 30-249 

 30-336 

 30-037 

 29-929 

 29-753 

 B 30-077 



14 .30-155 



15 30-180 



16 30-369 



17 30-452 



18 30-406 

 19:30-146 

 20 30-054 

 21! 29 -784 

 22,30-019 

 23 30-090 

 24129-974 



25 29-978 



26 29-965 



In 

 29-815 

 29-829 

 29-82669 

 29 -609167 

 29-840,64 

 30-156 61 

 ! 30 -104 70 

 ,30-145 70 

 30-2637451 

 29-949 79,50 

 29-802 71 1 52 

 :29-682 70 55 

 30-03776'47 

 30-132 70 43 

 30-024,78,55 

 30-19173 41 

 30-364 73 40 

 30-329 61 1 45 

 30-010 65|54 

 129-888 62 49 

 (29-768 65 50 



115-0 



102-0 



95-0 



72-5 



96-0 



90.0 



105-0 



102-0 



105-5 



46-5 

 49-5 

 42-0 

 51-5 

 46-5 

 40-5 

 36-5 

 43-5 

 51-0 

 110-048-0 



91 



29-984 74 1 50 

 29-989 75 47 



29-925 

 29-915 

 29-959 

 30-283 



29-767 

 29-932 

 29-865 

 29-875 

 29-884 

 29-818 

 30-079 



69 55 

 59 49 

 63 50 

 6145 

 66 54 

 68 51 

 6651 



50-f 



79.5 52-5 



108-0 46-0 



60-046-0 



80-5.53-0 



109-0'40-5 



105-0 42-0 



66-5 45-5 



69-0 54 '0 



80-0|49-5 



99-0 50-0 



101 -5 j 50-0 



110-0,47-5 



96-054 -0 



88-0 45-0 



88-0 49-5 



97-045-5 



102-5 49-0 



85-0 43-5 



68-0 48-5 



Wind. 



o 



NWNE SW 



SWS SW 



NW N 



NW W 



NW WSW 



NWSW 



NW NE SE 



SWNS 



NW SE 



NWE 



WNWN 



NW 

 W NW SE 

 NW NE E 

 W NW W 



NE E 



NWNESW 



NW SE NE 



SENSE 



NWNSE 



NW SE 



NW SE 



NW NE 



NE ESW 



NW 

 NWWN 

 SE W NW 

 SWSE W 

 NWN W 

 SW SE SW 





0-31 



26 

 •26! 



•26 0.25 

 10-02 

 26 0-14 

 .52 1 

 '52' 



•52 0-22 

 •86 0-03 

 •64 



•33 0-05 

 •78 



•78 



Total force 56 -46 1-02 



Tlie mean in all cases is taken from tlie siims 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 

 102 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 con-ect. 



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 obtainiDg the difference fro5?> 

 the average. 



