Guadalupe Island Cloud Trail
Guadalupe Island Cloud Trail
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瓜达卢佩岛云径
DOI：
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发表时间：
1994
期刊：
影响因子：
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通讯作者：
C. Dorman
中科院分区：
文献类型：
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作者：
C. Dorman
摘要在瓜达拉哈拉岛背风面观测到云的形成，云的形成是一种特殊的事件序列。一个云是一个狭窄的线性云，200公里长，不可能是平流。相反，一个透明的线性尾流平流顺风。之后，天气尺度的辐合导致尾迹凝结，形成线性云迹。这种弱天气尺度的变化可能导致线性云迹，对理解船舶云迹具有重要意义。
Abstract Clouds were observed forming in the lee of Guadalupe Island under a special sequence of events. One cloud was a narrow, linear cloud, 200 km long, that could not have been advected. Instead, a transparent linear wake was advected downwind. Later, synoptic-scale convergence caused the wake to condense, forming the linear cloud trail. That weak synoptic-scale variation may cause a linear cloud trail and has important implications for understanding ship cloud trails.