ON THE COASTS OF IRELAND. 99 



mean of all the values of Aq at that place, and have set down the excess as an irregu- 

 larity in the general height of the water at that place on that day. The numbers for 

 Courtown are taken by anticipation from Section XVII. The results are contained 

 in the following Table. With the view of ascertaining any possible connexion of these 

 irregularities with the cause of the winds, I have set down in the last columns the 

 character of the winds observed at the four stations Kilbaha, Port Rush, Kingstown, 

 and Passage West, which may be considered as nearly equidistant on the coast. [The 

 letter c attached to the letters describing the direction of the wind denotes that it 

 was nearly calm ; the letter s denotes that the wind was strong.] 



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