One might say this was a bell weather day for the Sierra Nevada
mountains. In January, just as the Sun was setting above the district of Albayzín in Grenada, Spain, a huge cloud appeared as a
bell capping the Veleta peak. Such
a Cap
cloud is formed by air forced upwards by a mountain
peak, with the air then cooling,
saturating with moisture, and finally having its molecular
water condense into cloud droplets. Such a
bell-shaped cloud
structure is unusual as air typically moves horizontally, making most clouds nearly
flat across at the bottom. Vertical waves can also give additional lenticular cloud layers, as also seen above. Given the
fleeting extent of the great cloud coupled with momentarily excellent sunset coloring, one might considered this also a bellwether day for an
accomplished photographer.
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