(It's not spittle...it's just water... falling!!!) |
Koumoulenn! (cloud)
The Cirrocumulus clouds that float at more than 6000m are formed when convection occurs. The water droplets then proceed to cool very quickly and may eventually freeze into ice crystals to form Cirrostratus clouds.
Avel (wind)
The convection conditions (that helped create the Cirrocumulus clouds above) were a result of the daytime sea-breezes blowing cool air onshore (from high to low pressure) over the comparatively warm land. Bretagne lies right on the convergence of a High pressure cell and a low pressure cell, constantly stirring the air around.
Avel & Dour= Koumoulenn
Hañv/Goañv (summer/winter)
As mentioned in a previous blog, Bretagne is at 47˚N. Despite the high latitude (equivalent to Nova Scotia), Bretagne has moderate Summers and Winters. In this case, the North Equatorial Current, Gulf Stream, and North Atlantic Drift keep the region warm; and, the north western winds (known as "noroît" in French, and "gwalarn" in Breton) keep the region cool.
Arnev (storm) diorren (develop) Gwezenn Forest* (tree forest)
*(redundant, I know, but the word "forest" lacked zing)
Den (human)
Bretagne has a long history of sailors. This is unsurprising as the region consists mostly of coast; but, now, with an understanding of the winds and currents that surround the area I understand the reason War was so often waged against the Bretons by mainland France. The strategic of the location as a main port of worldwide trade through much of the middle ages allowed France to become a powerful country.
Fin!
Works Cited: