The hydrometeor partitioning and microphysical processes over the Pacific Warm Pool in numerical modeling Atmospheric Research
收藏NOAA Institutional Repository2024-03-19 更新2026-04-25 收录
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https://doi.org/10.1016/j.atmosres.2016.09.009
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资源简介：
Numerical modeling is conducted to study the hydrometeor partitioning and microphysical source and sink processes during a quasi-steady state of thunderstorms over the Pacific Warm Pool by utilizing the microphysical model WISCDYMM to simulate selected storm cases. The results show that liquid-phase hydrometeors dominate thunderstorm evolution over the Pacific Warm Pool. The ratio of ice-phase mass to liquid-phase mass is about 41%: 59%, indicating that ice-phase water is not as significant over the Pacific Warm Pool as the liquid water compared to the larger than 50% in the subtropics and ~ 80% in the US High Plains in a previous study. Sensitivity tests support the dominance of liquid-phase hydrometeors over the Pacific Warm Pool. Grant no. NA10NES4400013
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NOAA
创建时间：
2024-03-19
