Explanation: Normal cloud bottoms a

Explanation: Normal cloud bottoms are flat. This is because moist warm air that rises and cools will condense into water droplets at a specific temperature, which usually corresponds to a very specific height. As water droplets grow, an opaque cloud forms. Under some conditions, however, cloud pockets can develop that contain large droplets of water or ice that fall into clear air as they evaporate. Such pockets may occur in turbulent air near a thunderstorm. Resulting mammatus clouds can appear especially dramatic if sunlit from the side. These mammatus clouds were photographed over Regina, Saskatchewan, Canada during the past summer.

Information from: APOD

Image Credit & Licence: Craig Lindsay, Wikipedia

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Explanation: Normal cloud bottoms are flat. This is because moist warm air that rises and cools will condense into water droplets at a specific temperature, which usually corresponds to a very specific height. As water droplets grow, an opaque cloud forms. Under some conditions , however, cloud pockets can develop that contain large droplets of water or ice that fall into clear air as they evaporate. Such pockets may occur in turbulent air near a thunderstorm. Resulting mammatus clouds can appear especially dramatic if sunlit from the side. These mammatus clouds were photographed over Regina, Saskatchewan, Canada during the past summer. Information from: APOD Image Credit & Licence: Craig Lindsay, Wikipedia

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解释：正常云彩底部是平的。这是，因为上升并且冷却的潮湿温暖的空气将凝聚入水滴在一个具体温度，通常对应于非常详细的高度。当水滴增长，一朵不透明的云彩形成。然而，在某些条件下包含大小滴水或冰落入晴空的云彩口袋可能开发，当他们蒸发。这样口袋在动荡空气也许发生在雷暴附近。发生的mammatus云彩可能看上去特别剧烈，如果被日光照射了从边。这些mammatus云彩被拍摄了在雷日纳，萨斯喀彻温省，加拿大在过去summer.

Information时从：APOD

画象着作权&执照：克雷格林赛，维基百科

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