From the information I received, I have reason to believe that the rainy season sets in usually about the first of July and continues very wet till September or October, when there is usually a dry fine season of a month or six weeks. I resided in the county of Cork, etc., from October till March, and found the winter much more soft and mild than ever I experienced one in England. I was also a whole summer there (1778), and it is fair to mention that it was as fine a one as ever I knew in England, though by no means so hot. I think hardly so wet as very many I have known in England. The tops of the Galty mountains exhibited the only snow we saw; and as to frosts, they were so slight and rare that I believe myrtles, and yet tenderer plants, would have survived without any covering. But when I say that the winter was not remarkable for being wet, I do not mean that we had a dry atmosphere. The inches of rain which fell in the winter I speak of would not mark the moisture of the climate. As many inches will fall in a single tropical shower as in a whole year in England. See Mitchel's "Present State of Great Britain and North America." But if the clouds presently disperse, and a bright sun shines, the air may soon be dry. The worst circumstance of the climate of Ireland is the constant moisture without rain. Wet a piece of leather, and lay it in a room where there is neither sun nor fire, and it will not in summer even be dry in a month. I have known gentlemen in Ireland deny their climate being moister than England, but if they have eyes let them open them, and see the verdure that clothes their rocks, and compare it with ours in England--where rocky soils are of a russet brown however sweet the food for sheep. Does not their island lie more exposed to the great Atlantic; and does not the west wind blow three-fourths of a year? If there was another island yet more westward, would not the climate of Ireland be improved? Such persons speak equally against fact, reason, and philosophy. That the moisture of a climate does not depend on the quantity of rain that falls, but on the powers of aerial evaporation, Dr. Dobson has clearly proved. "Phil. Trans." vol. lxvii., part i., p. 244. Oppression.