山东夏季暴雨对青藏高原东南部及邻近区域春季大气热源变化的响应
Response of summer rainstorm in Shandong Province to change of spring atmospheric heat sources in southeastern Tibet Plateau and its adjacent areas
山东夏季暴雨对青藏高原东南部及邻近区域春季大气热源变化的响应 |
| 焦洋, 张永婧, 尹承美, 褚颖佳 |
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Response of summer rainstorm in Shandong Province to change of spring atmospheric heat sources in southeastern Tibet Plateau and its adjacent areas |
| JIAO Yang, ZHANG Yongjing, YIN Chengmei, CHU Yingjia |
| 图4 春季高原大气热源强度指数回归的夏季200 hPa位势高度场（a,单位：gpm）和500 hPa位势高度场（填色区,单位：gpm）及整层水汽通量场（矢量,单位：g·cm-1·s-1）（b） |
| Fig.4 The 200 hPa geopotential height field （a, Unit： gpm）, 500 hPa geopotential height （color shaded areas, Unit： gpm）and integrated water vapor flux （vectors, Unit： g·cm-1·s-1） field （b） in summer regressed by spring atmospheric heat source intensity index over the Tibetan Plateau |
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