Uncertainty in weather and climate prediction. [PDF]
Slingo J, Palmer T.
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Intercomparison of methods of coupling between convection and large-scale circulation: 2. Comparison over nonuniform surface conditions. [PDF]
Daleu CL +13 more
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High-resolution NU-WRF simulations of a deep convective-precipitation system during MC3E: Further improvements and comparisons between Goddard microphysics schemes and observations. [PDF]
Tao WK +6 more
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Madden-Julian Oscillation analog and intraseasonal variability in a multicloud model above the equator. [PDF]
Majda AJ, Stechmann SN, Khouider B.
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The deepwater oxygen deficit in stratified shallow seas is mediated by diapycnal mixing. [PDF]
Rippeth T +6 more
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Assessing the Grell-Freitas Convection Parameterization in the NASA GEOS Modeling System. [PDF]
Freitas SR +6 more
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Relationships between radiation, clouds, and convection during DYNAMO. [PDF]
Ciesielski PE +4 more
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Temperature and residence time controls on an estuarine harmful algal bloom: Modeling hydrodynamics and Alexandrium fundyense in Nauset estuary. [PDF]
Ralston DK +4 more
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Vertical structure and modulation of TOGA COARE convection: a radar perspective
Tropical convection is an important component of the general circulation due to its role in driving large scale circulations which redistribute energy received at the equator to higher latitudes. The behavior of these large scale circulations is sensitive to the vertical distribution of diabatic heating produced by mesoscale precipitation system, which
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Convection in TOGA COARE: horizontal scale, morphology, and rainfall production
Shipboard radar data collected during the recent Tropical Oceans - Global Atmospheres Coupled Ocean - Atmosphere Response Experiment (TOGA COARE) provided an unprecedented view of convection in the western Pacific warm pool, a region of global climatological significance.
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