C 
he fuppofes to be commonly a Sign of Change of 
the Wind: But he does not inform us by what Me- 
thod he determin'd their Heights or Velocities. The 
reigning Wind, and general Strength of it, is noted 
at the End of each Month $ the Eclipfes alfo, and 
the Times of the New Moons; which he obferves 
make it appear, that the Notion of the Change of 
Weather depending on the Age of the Moon, is with- 
out any Ground : With other Mifcellaneous Obfem- 
tionsf as the Aurora Borealis , Fruitfulnefs or Sterility 
of the Scafon. He had no Thermometer. 
That from Hudickpvall in Sweden , by Mr. OTave 
Broman , fhews the Height of the Barometer fome- 
times once, fometimes twice or thrice a Day, O. S. 
in Englifb Meafure, with the Winds, and the Strength 
of them, and the Weather. There is alfo to the 
Diary 1729, annex'd an Account of the Height of 
the Sea- water for every Day, which I obferve varies in 
the whole about two Inches, and is fometimes inter- 
rupted by Floods from Rain. This, I fuppofe, may 
relate to the Tides in the Gulph of Bothnia, I have 
not inferred thefe in the Tables, not being of general 
Ufe- There is no Thermometer, nor the Quantity of 
Rain, fet down. 
That from Rifinge in Oftrogothia in Sweden , by 
Sueno Lam elans y Paftor and Provoft, gives the Height 
of the Barometer for the moft part three times, fome- 
times Eve times a Day, with the Hour of theObferva- 
tions, 0,S, in English Meafure. He refers for the 
Defcriptions of his Barometer and Thermometer to 
the Diary 1727. The Winds, with the Degree of their 
Strength, Weather, and Depth of Rain, are alfo fet 
down. 
In 
