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TitleSetnameType
101 Temporal and spatial analyses of pressure perturbations from the usarray transportable arrayir_etdText
102 Top-down constraints on CO emissions from wildfire inventories using a receptor-oriented Lagrangian particle dispersion modelir_etdText
103 Topographic effects on nighttime cooling in a basin and plain atmosphereir_etdText
104 Toward improved constraints on methane emissions from oil and natural gas fieldsir_etdText
105 Towards understanding the interaction between ozone and the circulation in the stratosphereir_etdText
106 Tracking and verification of tropical cyclone development in global ensemble prediction systems: evaluations during recent field programsir_etdText
107 Tropical cyclone intensity change: evaluating the effects of inner core precipitation properties and environmental influencesir_etdText
108 Tropical oceanic thunderstorms and the roles of evolution, organization, and environmental forcing in their electrificationir_etdText
109 Using a bimodal size distribution to retrieve marine low cloud properties using A-Train satellite and ground datair_etdText
110 Using an optimal estimation algorithm to describe the mass-dimensional properties of ice cloudsir_etdText
111 Using tropical warm pool-international cloud experiment observations to evaluate and improve high resolution simulations of tropical convective precipitation systemsir_etdText
112 Validation of mountain precipitation forecasts from the NCAR convection-permitting ensemble and operational forecast systems over the Western United Statesir_etdText
113 Variations in surface albedo arising from flooding and desiccation cycles on the playa surfaces of the Bonneville Salt Flats, Utahir_etdText
114 Variations of optical and radio lighting caracteristics and the relationship between storm convective intensity and above-cloud electric fieldsir_etdText
115 Verification of national weather service spot forecasts using surface observationsir_etdText
116 Which environmental conditions and core precipitation characteristics led to the rapid intensification of Hurricane Earl (2010)?ir_etdText
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