新西兰上空的Asperitas云
(原标题: Asperitas Clouds Over New Zealand)
2025-08-17
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这些是什么样的云?虽然它们的原因目前尚不清楚,但这种不寻常的大气结构,虽然看起来很危险,但似乎并不是气象末日的预兆。直到去年才被正式认定为一种独特的云类型,asperitas云的外观令人惊叹,罕见,而且相对来说还没有被研究过。虽然大多数低空云甲板底部是平坦的,但竖云的下面似乎有明显的垂直结构。因此,推测认为,阿斯米塔云可能与山附近形成的透镜状云有关,或者与雷暴有关的乳状云,或者可能是焚风——一种从山上流下的干燥向下的风。这种被称为“坎特伯雷拱”风的云向新西兰南岛东海岸移动。这张特色照片拍摄于2005年新西兰坎特伯雷的汉默泉,画面非常细致,部分原因是阳光从侧面照亮了起伏的云层。
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What kind of clouds are these? Although their cause is presently unknown, such unusual atmospheric structures, as menacing as they might seem, do not appear to be harbingers of meteorological doom. Formally recognized as a distinct cloud type only last year, asperitas clouds can be stunning in appearance, unusual in occurrence, and are relatively unstudied. Whereas most low cloud decks are flat bottomed, asperitas clouds appear to have significant vertical structure underneath. Speculation therefore holds that asperitas clouds might be related to lenticular clouds that form near mountains, or mammatus clouds associated with thunderstorms, or perhaps a foehn -- a type of dry downward wind that flows off mountains. Clouds from such a wind called the Canterbury arch stream toward the east coast of New Zealand's South Island. The featured image, taken above Hanmer Springs in Canterbury, New Zealand in 2005, shows great detail partly because sunlight illuminates the undulating clouds from the side.
© Witta Priester