( ) 
REMARKS on the foregoing tfA B LES. 
In that for the 2 "ear J707. 
I. T Obferve there is a great Agreement between the 
A Barometers at Coventry and Upmhifier, in their 
Ri/hig and Falling near the fame Time, at lead not 
many Hours before or after one another, and for the 
mod Part in the fame Proportion. Alfo when one is 
Stationary, the other is fo too, efpecially if of any 
Continuance : But at Coventry the Mercury is lower 
than at Upminfier about a tenth of an Inch, the Situ. 
* ation at Coventry being, I fuppofe, higher than that 
of Upminjler about Feet, according to my Experi- 
ments in Philof. franf. Numb. 13 6. 
II. I obferve alfo a greater Conformity between the 
Winds, than (confidering the Caufes of their perpetu- 
al Change) would be imagined. For although they 
may vary a Point or two, yet generally through all 
the eight Months, they tended nearly towards the 
fame Point of the Compafs, and changed in one Place 
as they did in the other 3 efpecially when they blew 
drongly, or were of fome Continuance. I have ob- 
ferved, that a Storm in one Place is fo in the other 3 
of which the Diaries at large give many Examples j 
and in this Table of 1707, in the Months of Septem- 
ber and OBoher , where Mr. Beighton hath noted 
the Winds Strength to be three and four, it is about 
the fame Strength with mine of five, fix, fevenand 
eight, I taking in more Degrees of the Strength of 
the Winds than he. 
III. I obferve alfo, that the Weather in each Place 
is for the mod Part nearly the fame. 
• a IV. I 
