Why Batch-0042-004 Establishes That Atmospheric Aerosol Hygroscopic Growth Modifies Radar Reflectivity Profiles in Stratocumulus Cloud Layers

为何批次0042-004确立大气气溶胶吸湿增长会改变层积云层的雷达反射率剖面

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Radar reflectivity profiles in marine stratocumulus clouds deviate systematically from Mie-scattering predictions due to aerosol-induced hygroscopic growth below cloud base.
In-situ aircraft measurements show that NaCl-rich sea spray particles swell up to 2.7× their dry diameter at 92% RH, altering dielectric contrast with ambient air.

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