Meteorological Objervations. 623 
remarkable warmth took place, in the midf of 
great falls of rain, for about three weeks after. 
I with to obferve farther, that on infpecting 
the ftate of the barometer, thermometer, and 
falls, during the year 1793 (which has been 
made out as accurately as my time and leifure 
would permit) it) will appear that’ every aber- 
ration of the barometer has been, accompanied 
or followed by:an evident deviation of tem- 
perature above er, below the medium of the 
feafon, taken together with a greater or leffer 
extent of falls; and is, if, not completely anfwered 
during the month, or in the commencement of 
the next, always, fufficiently compenfated for 
at fome diftance. It alfo appears that this rule 
may be depended on, viz. that when a change 
of weather, either to good or bad, has been 
indicated by undoubted figns, and is impend- 
ing; the longer it is delayed, the more com- 
plete it will be whenever it commences. ‘Thus 
we find the height of the barometer in Ja- 
nuary not being completely anfwered in that 
month, that in. February the heat that was 
owing enfued, notwithftanding the lownefs of 
the barometer; which again feems to haye 
been fully anfwered by the extent of falls. ..In 
March, the cold and falls being more than 
proportionate to the ftate of the barometer, 
warm or fair weather was therefore due. This 
however 
