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How Lenticular Clouds Form When Wind Flows Over Mountain Ridges
透镜状云如何在山脊上方气流中形成
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Lenticular clouds form when stable, moist air flows over mountains and creates standing waves.当稳定湿润的空气流经山脉时,会形成驻波,从而产生透镜状云。
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At the wave crest, air cools and condenses into smooth, lens-shaped cloud layers.在波峰处,空气冷却并凝结成光滑的透镜状云层。
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These clouds appear stationary despite strong winds because new moisture constantly replaces evaporated droplets.尽管风力强劲,这些云却看似静止不动,因为不断有新水汽补充蒸发掉的云滴。
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They often stack vertically like pancakes when multiple wave levels exist in the atmosphere.当大气中存在多个波动层时,它们常如煎饼般垂直堆叠。
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Photographers love them for their surreal, UFO-like appearance against clear skies.摄影师喜爱它们在晴朗天空下呈现的超现实、飞碟般的外观。
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Meteorologists use lenticular clouds as visual indicators of strong upper-level winds.气象学家将透镜状云视为高空强风的直观标志。
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Unlike storm clouds, they contain little vertical motion and rarely produce precipitation.与雷暴云不同,它们内部垂直运动微弱,极少产生降水。
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Their formation requires precise wind speed, humidity, and atmospheric stability conditions.其形成需要风速、湿度和大气稳定性等条件精确匹配。
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Pilots treat them as warning signs of severe turbulence in the lee of mountains.飞行员将其视为山背侧严重湍流的警示信号。
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Studying them helps refine mountain-wave forecasting models used in aviation safety.研究它们有助于改进用于航空安全的山地波预报模型。