ARTICLEhttps://test-journals.ametsoc.org/view/journals/wefo/2/1/1520-0434_1987_002_0070_asomvm_2_0_co_2.xmlA Study of 500 mb Vorticity Maxima Crossing the East Coast of North America and Associated Surface Cyclogenesis2020-12-07https://test-journals.ametsoc.org/view/journals/wefo/2/1/1520-0434_1987_002_0070_asomvm_2_0_co_2.pdf2020-12-08A Study of 500 mb Vorticity Maxima Crossing the East Coast of North America and Associated Surface Cyclogenesishttps://test-journals.ametsoc.org/view/journals/wefo/2/1/1520-0434_1987_002_0017_tdossv_2_0_co_2.xmlThe Diagnosis of Synoptic-Scale Vertical Motion in an Operational Environment2020-12-07https://test-journals.ametsoc.org/view/journals/wefo/2/1/1520-0434_1987_002_0017_tdossv_2_0_co_2.pdf2020-12-08The Diagnosis of Synoptic-Scale Vertical Motion in an Operational Environmenthttps://test-journals.ametsoc.org/view/journals/wefo/2/1/1520-0434_1987_002_0032_dwciw_2_0_co_2.xmlDerechos: Widespread Convectively Induced Windstorms2020-12-07https://test-journals.ametsoc.org/view/journals/wefo/2/1/1520-0434_1987_002_0032_dwciw_2_0_co_2.pdf2020-12-08Derechos: Widespread Convectively Induced Windstormshttps://test-journals.ametsoc.org/view/journals/wefo/2/1/1520-0434_1987_002_0050_tuaion_2_0_co_2.xmlThe Use and Interpretation of Numerical Weather Prediction Model Output in Identifying Synoptic-Scale Environments Associated with Development of Mesoscale Convective Systems2020-12-07https://test-journals.ametsoc.org/view/journals/wefo/2/1/1520-0434_1987_002_0050_tuaion_2_0_co_2.pdf2020-12-08The Use and Interpretation of Numerical Weather Prediction Model Output in Identifying Synoptic-Scale Environments Associated with Development of Mesoscale Convective Systemshttps://test-journals.ametsoc.org/view/journals/wefo/2/1/1520-0434_1987_002_0003_tdblsa_2_0_co_2.xmlThe Distinction between Large-Scale and Mesoscale Contribution to Severe Convection: A Case Study Example2020-12-07https://test-journals.ametsoc.org/view/journals/wefo/2/1/1520-0434_1987_002_0003_tdblsa_2_0_co_2.pdf2020-12-08The Distinction between Large-Scale and Mesoscale Contribution to Severe Convection: A Case Study Example