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Polar vortex formation in giant planet atmospheres under moist convection
Published 2016“…We find that the type of shallow polar flow that occurs on a giant planet can be described by the size ratio of small eddies to the planetary radius and the energy density of its atmosphere due to latent heating from moist convection. …”
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Long-term variations of North Atlantic tropical cyclone activity downscaled from a coupled model simulation of the last millennium
Published 2015“…An alternative approach is to study long-term Atlantic TC variability within the framework of a coupled ocean-atmosphere climate model simulation. We have taken such an approach using a simulation of the National Center for Atmospheric Research Climate System Model 1.4 forced with estimated natural and anthropogenic forcing over the past millennium. …”
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Double benefit of limiting global warming for tropical cyclone exposure
Published 2021Get full text
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Estimating tropical cyclone precipitation risk in Texas
Published 2014“…This paper uses a new rainfall algorithm to simulate the long-term tropical cyclone precipitation (TCP) climatology in Texas based on synthetic tropical cyclones generated from National Center for Atmospheric Research/National Centers for Environmental Prediction reanalysis data from 1980 to 2010. …”
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A Linear Response Framework for Radiative-Convective Instability
Published 2020“…For Betts-Miller convection, the stability critically depend on a key parameter: the heating to advection of moisture conversion rate (HAM); warmer atmospheres with higher HAM exhibit more linear instability. …”
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Signature of microphysics on spatial rainfall statistics
Published 2014“…We examine this assertion by analysis of high-resolution simulations of an atmosphere in radiative-convective equilibrium performed using the Weather Research and Forecasting (WRF) model and prescribing different rain terminal velocity settings corresponding to small, slowly falling drops and large, quickly falling drops, respectively. …”
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The climate time scale in the approach to radiative-convective equilibrium
Published 2015“…We show that the size of τ[subscript C] is an intrinsic property of the coupling between the atmosphere and surface, and not a result of the thermal inertia of the surface alone. …”
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