[ ><So ] 
with their Strength, and the Weather, for the Year 
2730. The Medium of the Thermometer is taken 
from both the Evening and Morning Heights, the 
Difference there being very great in Proportion be- 
tween Morning and Evening. 
That from Bofton in New-England , by Baul 
i Dudley , Efq; F. R. S. {hews the Weather three times 
a Day, and Wind once or twice. No Barometer or 
Thermometer. 
There is one of the Year 1729, feems to be Swedijhy 
but finding neither the Author's Name nor Place, I 
have not inferted it. 
In the Year 1730, thofe from Crane-Comt , South - 
wick , Kent, Hudickfoall , OJlrogothia , Upfal , Svena- 
ker , Lunden , Betna , Wittemberg , Badua and Bofton , 
are continued in the fame Manner. There is none 
from Bygdea. The Obfervations for the Year 
1730, by Mr. ©. Sporing , fhew the Height of the 
Barometer twice a Day, in Swedijh Inches and Deci- 
mals, but the mean Heights are reduc'd to Englijh in 
the Tables. They fhew alfo the Winds and W eather, 
and in the laft Column the Aurora Boreales , which 
are frequent in moft Months of the Year. 
That from Naples , by Cyrillus, fhews the Height 
of the Thermometer, which is Mr. Hauksbees , once 
a Day. The Winds, with their Strength, and Wea- 
ther, and Depth of Rain in Neapolitan Meafures, 2 3 
of which make a London Inch, and are reduc'd there- 
to in the Tables. The Barometrical Heights he has 
not fet down,becaufe he found them not to agree with 
thofe of former Years, which made him fufpeft his In- 
ftrument to be out of Order; but as it appears he had 
remov’d his Habitation, it might be owing to its being 
fituated 
