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- W4386820753 abstract "Abstract The low air pressure and density over the Tibetan Plateau may have an impact on the microphysical features of rainfall. Using a two-dimensional video disdrometer (2DVD), a micro rain radar (MRR), and a microwave radiometer (MWR), the features of the raindrop size distribution (DSD) on the southeastern Tibetan Plateau (SETP) are explored and compared with those in low-altitude regions. The falling speed of raindrops on the SETP is higher than that in low-altitude areas. Under different rainfall rate categories, the number concentration and the maximum diameter of raindrops on the SETP are smaller than those in low-altitude region. The convective rainfall on the SETP is more maritime-like because the South Asian summer monsoon brings water vapor from the ocean here. For stratiform and convective rainfall, the SETP has more small-sized raindrops than low-altitude locations. The mass-weighted mean diameters (D m ) on the SETP are the smallest among six sites. The generalized intercept parameter (N w ) of stratiform rainfall is balanced at a low rainfall rate, while that of convective rainfall is balanced at a high rainfall rate. Furthermore, for a given μ (the shape parameter of Gamma distribution) value, the λ (the slope parameter of Gamma distribution) value on the SETP is the highest of the six sites." @default.
- W4386820753 created "2023-09-19" @default.
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- W4386820753 date "2023-09-18" @default.
- W4386820753 modified "2023-10-16" @default.
- W4386820753 title "Comparisons of Rainfall Microphysical Characteristics Between the southeastern Tibetan Plateau and Low-altitude Areas" @default.
- W4386820753 doi "https://doi.org/10.1175/jamc-d-23-0046.1" @default.
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