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首页> 外文期刊>SOLA: Scientific Online Letters on the Atmosphere >Changes of Baiu (Mei-yu) Frontal Activity in the Global Warming Climate Simulated by a Non-hydrostatic Regional Model
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Changes of Baiu (Mei-yu) Frontal Activity in the Global Warming Climate Simulated by a Non-hydrostatic Regional Model

机译：用非静水区域模型模拟的全球变暖气候中Bau（Mei-yu）额叶活动的变化

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References(12) Cited-By(22) Supplementary materials(1) The Baiu (Mei-yu) front over East Asia in the global warming climate as well as that in the present one, is studied using outputs of a non-hydrostatic regional model with a horizontal grid size of 5 km (NHM). The NHM was run in June and July for ten years, applying a spectral boundary coupling method to reduce the horizontal phase differences of large-scale disturbances using the outputs of a global climate model with a grid size of 20 km. In the global warming climate, the Baiu front is likely to stay over the southern Japan Islands around the latitudes of 30 N-32 N and will not move northward. Therefore, the activity of the Baiu front maintains longer than that in the present climate, and the precipitation increases. On the other hand, the precipitation decreases over the northern Japan Islands and the northern Korean Peninsula. Years with no end of the Baiu season are often seen, and the frequency of occurrence of heavy rainfall greater than 30 mm h-1 increases over the Japan Islands.
机译：参考文献（12）被引用的文献（22）补充材料（1）使用非静水区域的输出来研究全球变暖气候以及当前气候中东亚的Baiu（Mei-yu）锋面模型的水平网格大小为5 km（NHM）。 NHM在6月和7月运行了十年，应用了一种频谱边界耦合方法，以一个具有20 km网格大小的全球气候模型的输出来减少大规模干扰的水平相位差。在全球气候变暖的情况下，Baiu锋很可能会停留在30 N-32 N纬度的日本南部岛屿上方，并且不会向北移动。因此，与当前气候相比，Baiu锋的活动时间更长，并且降水增加。另一方面，日本北部诸岛和朝鲜半岛北部的降水减少。通常会看到Baiu季节没有结束的年份，并且在日本诸岛上，强降雨的发生频率大于30 mm h-1。

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