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Assessing the impact of the Kuroshio Current on vertical cloud structure using CloudSat data

机译:使用CloudSat数据评估黑潮对垂直云结构的影响

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This study analyzed CloudSat satellite data to determine how the warm ocean Kuroshio Current affects the vertical structure of clouds. Rainfall intensity around the middle troposphere (6?km in height) over the Kuroshio was greater than that over surrounding areas. The drizzle clouds over the Kuroshio have a?higher frequency of occurrence of geometrically thin (0.5–3?km) clouds and thicker (7–10?km) clouds compared to those around the Kuroshio. Moreover, the frequency of occurrence of precipitating clouds with a?geometric thickness of 7?to 10?km increased over the Kuroshio. Stronger updrafts over the Kuroshio maintain large droplets higher in the upper part of the cloud layer, and the maximum radar reflectivity within a cloud layer in non-precipitating and drizzle clouds over the Kuroshio is higher than that around the Kuroshio.
机译:这项研究分析了CloudSat卫星数据,以确定温暖的海洋黑潮洋流如何影响云的垂直结构。黑潮上空对流层中部(高度6?km)周围的降雨强度大于周围地区。与黑潮周围的云相比,黑潮上的细雨云的发生频率更高,在几何上稀疏的云(0.5–3?km)和较厚的云(7–10?km)的发生频率更高。此外,在黑潮上,几何厚度为7?至10?km的降水云的出现频率增加了。黑潮上空较强的上升气流使云层上部的大液滴保持较高,黑潮上空的无雨云和细雨云的云层内的最大雷达反射率高于黑潮周围。

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