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Part I: Measures of Predictabilityhttps://test-journals.ametsoc.org/view/journals/atsc/61/20/1520-0469_2004_061_2441_aosspo_2.0.co_2.xmlApproximation of Single Scattering Properties of Ice and Snow Particles for High Microwave Frequencies2026-10-25https://test-journals.ametsoc.org/view/journals/atsc/61/20/1520-0469_2004_061_2441_aosspo_2.0.co_2.pdf2026-10-25Approximation of Single Scattering Properties of Ice and Snow Particles for High Microwave Frequencieshttps://test-journals.ametsoc.org/view/journals/atsc/61/20/1520-0469_2004_061_2457_caadts_2.0.co_2.xmlCan Anthropogenic Aerosols Decrease the Snowfall Rate?2026-10-25https://test-journals.ametsoc.org/view/journals/atsc/61/20/1520-0469_2004_061_2457_caadts_2.0.co_2.pdf2026-10-25Can Anthropogenic Aerosols Decrease the Snowfall Rate?https://test-journals.ametsoc.org/view/journals/atsc/61/20/1520-0469_2004_061_2469_roaodp_2.0.co_2.xmlRetrieval of Atmospheric Optical Depth Profiles from Downward-Looking High-Resolution O2 A-Band Measurements: Optically Thin Conditions2026-10-25https://test-journals.ametsoc.org/view/journals/atsc/61/20/1520-0469_2004_061_2469_roaodp_2.0.co_2.pdf2026-10-25Retrieval of Atmospheric Optical Depth Profiles from Downward-Looking High-Resolution O2 A-Band Measurements: Optically Thin Conditionshttps://test-journals.ametsoc.org/view/journals/atsc/61/20/1520-0469_2004_061_2478_doteoa_2.0.co_2.xmlDerivation of the Equations of Atmospheric Motion in Oblate Spheroidal Coordinates2026-10-25https://test-journals.ametsoc.org/view/journals/atsc/61/20/1520-0469_2004_061_2478_doteoa_2.0.co_2.pdf2026-10-25Derivation of the Equations of Atmospheric Motion in Oblate Spheroidal Coordinates