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A) Raindrops are not tear-shaped, as most people think. B) Very small raindrops are almost spherical in shape. C) Larger raindrops become flattened at the bottom, like that of a hamburger bun, due to air resistance. D) Large raindrops have a large amount of air resistance, which makes them begin to become unstable.
Illustration from Daisies and Raindrops. Daisies and Raindrops is an illustrated collection of short stories and poems for children by Amy Ella Blanchard. It was first published in 1882 by E.P. Dutton. [1] This book contains excellent examples of children's illustrations from the "Golden Age" of illustration.
During shower activity raindrops cover the entire surface, whereas raindrop impressions are generally scattered and few in number. Because the rain is falling "everywhere," raindrop impressions should occur equally on sand-sized material as well as mud, yet in the geologic record these impressions are largely confined to fine-grained rock.
The raindrop size distribution (DSD), or granulometry of rain, is the distribution of the number of raindrops according to their diameter (D).Three processes account for the formation of drops: water vapor condensation, accumulation of small drops on large drops and collisions between sizes.
Light rays enter a raindrop from one direction (typically a straight line from the Sun), reflect off the back of the raindrop, and fan out as they leave the raindrop. The light leaving the rainbow is spread over a wide angle, with a maximum intensity at the angles 40.89–42°.
If this layer of subfreezing air is sufficiently deep, the raindrops may have time to freeze into ice pellets (sleet) before reaching the ground. However, if the subfreezing layer of air at the surface is very shallow, the rain drops falling through it will not have time to freeze and they will hit the ground as supercooled rain. When these ...
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