It's all that warm water out there in the North Atlantic. The air moves across it from the west, soaking up moisture like a paper towel moving across a wet kitchen counter, to wring itself out on Ireland's west coast.
Geochemist Wally Broecker imagines a globe-spanning oceanic conveyor belt with its northern terminus near Iceland. Cold winds from Canada blow across the water there, cooling it. The cold, dense water sinks, and flows as a deep bottom current southward around the Cape of Good Hope into the Indian and Pacific oceans. There it rises, warms, and as a shallower current returns to the Atlantic and flows northwards.
Near Iceland, this water from a tropic sea finds its way to the surface where its heat is stolen away by Canadian winds. These are the balmy, moisture-drenched westerlies that warm and wet Ireland.
So, if Broecker is right, Ireland's green damp has its origin in palm-fringed oceans on the other side of the world.
But occasionally, every tenth summer or so, a high pressure ridge drifts up from the Azores and sits for weeks upon Ireland like a sunny crown. We are having a brilliant streak of grand weather now -- perfect for yesterday's Ventry Regatta.
