ARTICLEhttps://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0281_ahpsla_2_0_co_2.xmlA High Plains Squall Line Associated with Severe Surface Winds2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0281_ahpsla_2_0_co_2.pdf2026-10-20A High Plains Squall Line Associated with Severe Surface Windshttps://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0303_acogwa_2_0_co_2.xmlA Climatology of Gravity Waves and Other Coherent Disturbances at the Boulder Atmospheric Observatory during March–April 19842026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0303_acogwa_2_0_co_2.pdf2026-10-20A Climatology of Gravity Waves and Other Coherent Disturbances at the Boulder Atmospheric Observatory during March–April 1984https://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0330_odtdmo_2_0_co_2.xmlOne-Dimensional Time-Dependent Modeling of GATE Cumulonimbus Convection2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0330_odtdmo_2_0_co_2.pdf2026-10-20One-Dimensional Time-Dependent Modeling of GATE Cumulonimbus Convectionhttps://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0353_dpiasg_2_0_co_2.xmlDynamical Predictability in a Simple General Circulation Model: Average Error Growth2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0353_dpiasg_2_0_co_2.pdf2026-10-20Dynamical Predictability in a Simple General Circulation Model: Average Error Growthhttps://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0371_mamsoc_2_0_co_2.xmlMesoscale and Microscale Structure of Cirrus Clouds: Three Case Studies2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0371_mamsoc_2_0_co_2.pdf2026-10-20Mesoscale and Microscale Structure of Cirrus Clouds: Three Case Studieshttps://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0397_ubmdbe_2_0_co_2.xmlUnstable Baroclinic Modes Damped by Ekman Dissipation2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0397_ubmdbe_2_0_co_2.pdf2026-10-20Unstable Baroclinic Modes Damped by Ekman Dissipationhttps://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0402_lbiwtg_2_0_co_2.xmlLinear Baroclinic instability with the Geostrophic Momentum Approximation2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0402_lbiwtg_2_0_co_2.pdf2026-10-20Linear Baroclinic instability with the Geostrophic Momentum Approximationhttps://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0410_tspwsa_2_0_co_2.xmlThe Separated Polar Winter Stratopause: A Gravity Wave Driven Climatological Feature2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0410_tspwsa_2_0_co_2.pdf2026-10-20The Separated Polar Winter Stratopause: A Gravity Wave Driven Climatological Featurehttps://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0423_gwsbak_2_0_co_2.xmlGravity Wave Structure between 60 and 90 km Inferred from Space Shuttle Reentry Data2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0423_gwsbak_2_0_co_2.pdf2026-10-20Gravity Wave Structure between 60 and 90 km Inferred from Space Shuttle Reentry Datahttps://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0435_wsitaw_2_0_co_2.xmlWarm Stratopause in the Antarctic Winter2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/3/1520-0469_1989_046_0435_wsitaw_2_0_co_2.pdf2026-10-20Warm Stratopause in the Antarctic Winterhttps://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0441_iblass_2_0_co_2.xmlInteractions between Long and Synoptic-Scale Waves. Part I: Instability of a Nonzonal Flow2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0441_iblass_2_0_co_2.pdf2026-10-20Interactions between Long and Synoptic-Scale Waves. Part I: Instability of a Nonzonal Flowhttps://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0450_iblass_2_0_co_2.xmlInteractions between Long and Synoptic-Scale Waves. Part II: Growth Rate of Long Waves2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0450_iblass_2_0_co_2.pdf2026-10-20Interactions between Long and Synoptic-Scale Waves. Part II: Growth Rate of Long Waveshttps://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0460_eosfot_2_0_co_2.xmlEffect of Surface Fluxes on the Nonlinear Development of Baroclinic Waves2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0460_eosfot_2_0_co_2.pdf2026-10-20Effect of Surface Fluxes on the Nonlinear Development of Baroclinic Waveshttps://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0476_tmwoaa_2_0_co_2.xmlTropopausal Mountain Waves over Arecibo: A Case Study2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0476_tmwoaa_2_0_co_2.pdf2026-10-20Tropopausal Mountain Waves over Arecibo: A Case Studyhttps://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0489_aovnme_2_0_co_2.xmlApplication of Vertical Normal Mode Expansion to Problems of Baroclinic Instability2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0489_aovnme_2_0_co_2.pdf2026-10-20Application of Vertical Normal Mode Expansion to Problems of Baroclinic Instabilityhttps://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0511_rccbrb_2_0_co_2.xmlRadiative Cooling Calculated by Random Band Models with S-1-β Tailed Distribution2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0511_rccbrb_2_0_co_2.pdf2026-10-20Radiative Cooling Calculated by Random Band Models with S-1-β Tailed Distributionhttps://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0521_anioto_2_0_co_2.xmlA Numerical Investigation of the Organization and Interaction of the Convective and Stratiform Regions of Tropical Squall Lines2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0521_anioto_2_0_co_2.pdf2026-10-20A Numerical Investigation of the Organization and Interaction of the Convective and Stratiform Regions of Tropical Squall Lineshttps://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0545_tlsonm_2_0_co_2.xmlThe Linear Stability of Nonlinear Mountain Waves: Implications for the Understanding of Severe Downslope Windstorms2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0545_tlsonm_2_0_co_2.pdf2026-10-20The Linear Stability of Nonlinear Mountain Waves: Implications for the Understanding of Severe Downslope Windstormshttps://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0565_tlsonm_2_0_co_2.xmlThe Structure and Energetics of Transient Eddies in a Numerical Simulation of Breaking Mountain Waves2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0565_tlsonm_2_0_co_2.pdf2026-10-20The Structure and Energetics of Transient Eddies in a Numerical Simulation of Breaking Mountain Waveshttps://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0586_otscos_2_0_co_2.xmlOn the Structural Characteristics of Steady Finite-Amplitude Mountain Waves over Bell-Shaped Topography2026-10-20https://test-journals.ametsoc.org/view/journals/atsc/46/4/1520-0469_1989_046_0586_otscos_2_0_co_2.pdf2026-10-20On the Structural Characteristics of Steady Finite-Amplitude Mountain Waves over Bell-Shaped Topography