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Isaac M. Held

Researcher at Princeton University

Publications -  216
Citations -  40895

Isaac M. Held is an academic researcher from Princeton University. The author has contributed to research in topics: Climate model & Climate change. The author has an hindex of 88, co-authored 215 publications receiving 37064 citations. Previous affiliations of Isaac M. Held include Geophysical Fluid Dynamics Laboratory & Harvard University.

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Entropy Budget of an Atmosphere in Radiative–Convective Equilibrium. Part I: Maximum Work and Frictional Dissipation

TL;DR: In this article, the entropy budget of an atmosphere in radiative-convective equilibrium is analyzed, and the dominant irreversible entropy source is associated with irreversible phase changes and diffusion of water vapor.
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SST Forcings and Sahel Rainfall Variability in Simulations of the Twentieth and Twenty-First Centuries

TL;DR: In this paper, a statistical analysis of the preindustrial, twentieth-century and twenty-first-century A1B scenario simulations in the latest Coupled Model Intercomparison Project 3 (CMIP3) dataset is presented.
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The Surface Branch of the Zonally Averaged Mass Transport Circulation in the Troposphere

TL;DR: In this paper, the near-surface branch of the overturning mass transport circulation in the troposphere, containing the equatorward flow, is examined in isentropic and geometric coordinates.
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Aquaplanets, Climate Sensitivity, and Low Clouds

TL;DR: In this paper, the authors used two climate models to demonstrate that aquaplanets can successfully predict a climate model's sensitivity to an idealized climate change and found that tropical low clouds appear to play a leading role in determining the sensitivity.
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Equilibrium Atmospheric Response to North Atlantic SST Anomalies

TL;DR: In this paper, the equilibrium general circulation model (GCM) response to sea surface temperature (SST) anomalies in the western North Atlantic region is studied, where a coarse resolution GCM, with realistic lower boundary conditions including topography and climatological SST distribution, is integrated in perpetual January and perpetual October modes.