A single city can contain dozens of distinct microclimates, varying by as much as 10-15°F depending on location and features like sun exposure and building materials.elaborate
Cloud iridescence, those colorful patches in clouds, are caused by diffraction of light around tiny water droplets or ice crystals—similar to how a prism separates light into a rainbow, but on a much smaller scale.
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Crepuscular rays, those dramatic sunbeams that appear to radiate from the sun, are actually caused by shadows cast by clouds or other atmospheric particles.
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Climate graphs (climatographs) often use a double-y-axis, showing temperature and precipitation on separate scales, to better visualize their relationship throughout the year.
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