Meteorological Qbfervations. 319 



degree below it. The numbers therefore 

 which have no o before them, iignify the 

 upper degrees. Some examples will make 

 this ftill more intelligible. On the ijth 

 of December it is remarked, that the ther- 

 mometer, at eight o'clock in the morn- 

 ing, was at 02.5. It was therefore at 2 

 degrees and T S O-, or half a degree, below 

 the freezing-point ; but at two in the af- 

 ternoon, it was at oo.o, or exactly upon the 

 freezing-point. If it had been 00.3, it 

 v/ould have iignified that the thermometer 

 was fallen iV of a degree below the freezing- 

 point ; but 0.3 would fignify, that it was 

 rifen T 3 -o- of a degree above the freezing- 

 point. Thus likewife 03.0. is three de- 

 grees below the freezing-point; and 4.0. 

 four degrees above it. 



THE numbers in the columns of the 

 winds fignify as follows : o, is a calm ; 

 i, a gentle breeze ; 2, a frelh gale ; 3, a 

 ftrong gale ; and 4, a violent ftorm or bur-* 

 ricane. When, in fome of the laft tables, 

 the winds are only marked once a day, it 

 fignifies that they have not changed that 

 day. Thus, on the 2 ifl of December, ftands 

 N. o fair. This {hews that the weather- 

 cocks have turned to the north all day; 

 but that no wind has been felt, and the 

 fky has been clear all the day long. 



BEFORE 



