摘要 : Parameters of the normalized gamma particle size distribution (PSD) have been retrieved from the Precipitation Image Package (PIP) snowfall observations collected during the International Collaborative Experiment-PyeongChang Olym-... 展开 Parameters of the normalized gamma particle size distribution (PSD) have been retrieved from the Precipitation Image Package (PIP) snowfall observations collected during the International Collaborative Experiment-PyeongChang Olym-pic and Paralympic winter games (ICE-POP 2018). Two of the gamma PSD parameters, the mass-weighted particle diameter Dmass and the normalized intercept parameter NW, have median values of 1.15-1.31 mm and 2.84-3.04 log(mm21 m23), respec-tively. This range arises from the choice of the relationship between the maximum versus equivalent diameter, Dmx-Deq, and the relationship between the Reynolds and Best numbers, Re-X. Normalization of snow water equivalent rate (SWER) and ice water content W by NW reduces the range in NW, resulting in well -fitted power-law relationships between SWER/NW and Dmass and between W/NW and Dmass. The bulk descriptors of snowfall are calculated from PIP observations and from the gamma PSD with values of the shape parameterm ranging from 22 to 10. NASA's Global Precipitation Measurement (GPM) mission, which adopted the normalized gamma PSD, assumes m 5 2 and 3 in its two separate algorithms. The mean fractional bias (MFB) of the snowfall parameters changes with m, where the functional dependence on m depends on the specific snowfall parameter of interest. The MFB of the total concentration was underestimated by 0.23-0.34 when m 5 2 and by 0.29-0.40 when m 5 3, whereas the MFB of SWER had a much narrower range (from 20.03 to 0.04) for the same m values. 收起