ARTICLEhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0095_pitvos_2_0_co_2.xmlPATTERN IN THE VERTICAL OF SNOW GENERATION2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0095_pitvos_2_0_co_2.pdf2026-10-19PATTERN IN THE VERTICAL OF SNOW GENERATIONhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0115_rsorpm_2_0_co_2.xmlRAIN SCAVENGING OF RADIOACTIVE PARTICULATE MATTER FROM THE ATMOSPHERE2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0115_rsorpm_2_0_co_2.pdf2026-10-19RAIN SCAVENGING OF RADIOACTIVE PARTICULATE MATTER FROM THE ATMOSPHEREhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0126_tasjsd_2_0_co_2.xmlTHE ARCTIC STRATOSPHERIC JET STREAM DURING THE WINTER OF 1955–19562026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0126_tasjsd_2_0_co_2.pdf2026-10-19THE ARCTIC STRATOSPHERIC JET STREAM DURING THE WINTER OF 1955–1956https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0136_anotso_2_0_co_2.xmlA NOTE ON THE STABILITY OF BAROCLINIC WAVES2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0136_anotso_2_0_co_2.pdf2026-10-19A NOTE ON THE STABILITY OF BAROCLINIC WAVEShttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0141_vithtm_2_0_co_2.xmlVARIATIONS IN THE HIGH TROPOSPHERIC MEAN FLOW OVER AUSTRALIA AND NEW ZEALAND2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0141_vithtm_2_0_co_2.pdf2026-10-19VARIATIONS IN THE HIGH TROPOSPHERIC MEAN FLOW OVER AUSTRALIA AND NEW ZEALANDhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0150_boamae_2_0_co_2.xmlBUDGET OF ANGULAR MOMENTUM AND ENERGY IN TROPICAL CYCLONES2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0150_boamae_2_0_co_2.pdf2026-10-19BUDGET OF ANGULAR MOMENTUM AND ENERGY IN TROPICAL CYCLONEShttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0160_psohws_2_0_co_2.xmlPOWER SPECTRUM OF HORIZONTAL WIND SPEED IN THE FREQUENCY RANGE FROM 0.0007 TO 900 CYCLES PER HOUR2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0160_psohws_2_0_co_2.pdf2026-10-19POWER SPECTRUM OF HORIZONTAL WIND SPEED IN THE FREQUENCY RANGE FROM 0.0007 TO 900 CYCLES PER HOURhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0165_amoad_2_0_co_2.xmlAIRBORNE MEASUREMENTS OF ATOMIC DEBRIS2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0165_amoad_2_0_co_2.pdf2026-10-19AIRBORNE MEASUREMENTS OF ATOMIC DEBRIShttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0176_tiofoi_2_0_co_2.xmlTHE INFLUENCE OF FINITE OBSERVATION INTERVALS ON THE MEASUREMENT OF TURBULENT DIFFUSION PARAMETERS2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0176_tiofoi_2_0_co_2.pdf2026-10-19THE INFLUENCE OF FINITE OBSERVATION INTERVALS ON THE MEASUREMENT OF TURBULENT DIFFUSION PARAMETERShttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0182_smodsd_2_0_co_2.xmlSTAIN METHOD OF DROP-SIZE DETERMINATION2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0182_smodsd_2_0_co_2.pdf2026-10-19STAIN METHOD OF DROP-SIZE DETERMINATIONhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0184_acshss_2_0_co_2.xmlA COORDINATE SYSTEM HAVING SOME SPECIAL ADVANTAGES FOR NUMERICAL FORECASTING2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0184_acshss_2_0_co_2.pdf2026-10-19A COORDINATE SYSTEM HAVING SOME SPECIAL ADVANTAGES FOR NUMERICAL FORECASTINGhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0186_cotrbr_2_0_co_2.xmlCOMMENTS ON "THE RELATION BETWEEN RAINFALL WHOLE ARGUMENT ON THE CAUSES OF A 6- TO 7-YEAR RAINFALL AND METEOR SHOWERS" PERIODICITY2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0186_cotrbr_2_0_co_2.pdf2026-10-19COMMENTS ON "THE RELATION BETWEEN RAINFALL WHOLE ARGUMENT ON THE CAUSES OF A 6- TO 7-YEAR RAINFALL AND METEOR SHOWERS" PERIODICITYhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0187_c_2_0_co_2.xmlREPLY2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0187_c_2_0_co_2.pdf2026-10-19REPLYhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0188_cotsap_2_0_co_2.xmlCOMMENTS ON "THE SEMI-ANNUAL PRESSURE OSCILLATION, ITS CAUSE AND EFFECTS"2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0188_cotsap_2_0_co_2.pdf2026-10-19COMMENTS ON "THE SEMI-ANNUAL PRESSURE OSCILLATION, ITS CAUSE AND EFFECTS"https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0189_r_2_0_co_2.xmlREPLY2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0189_r_2_0_co_2.pdf2026-10-19REPLYhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0190_catawn_2_0_co_2.xmlCLEAR-AIR TURBULENCE ASSOCIATED WITH NEGATIVE VERTICAL WIND SHEAR2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0190_catawn_2_0_co_2.pdf2026-10-19CLEAR-AIR TURBULENCE ASSOCIATED WITH NEGATIVE VERTICAL WIND SHEARhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0191_r_2_0_co_2.xmlREPLY2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0191_r_2_0_co_2.pdf2026-10-19REPLYhttps://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0192_coswbu_2_0_co_2.xmlCRYSTALLIZATION OF SUPERCOOLED WATER BY ULTRASONIC IRRADIATION2026-10-19https://test-journals.ametsoc.org/view/journals/atsc/14/2/1520-0469_1957_014_0192_coswbu_2_0_co_2.pdf2026-10-19CRYSTALLIZATION OF SUPERCOOLED WATER BY ULTRASONIC IRRADIATION