Isaac M. Held
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View article: Convectively-Coupled Global Rossby Modes in an Idealized Moist GCM
Convectively-Coupled Global Rossby Modes in an Idealized Moist GCM Open
The westward-propagating convectively-coupled equatorial wave (CCEW) variability produced by an idealized general circulation model (GCM) is investigated.The model is a zonally-symmetric aquaplanet with a slab ocean.Water vapor in the mode…
View article: Forecasting Tropical Annual Maximum Wet‐Bulb Temperatures Months in Advance From the Current State of ENSO
Forecasting Tropical Annual Maximum Wet‐Bulb Temperatures Months in Advance From the Current State of ENSO Open
Humid heatwaves, characterized by high temperature and humidity combinations, challenge tropical societies. Extreme wet‐bulb temperatures (TW) over tropical land are coupled to the warmest sea surface temperatures by atmospheric convection…
View article: Forecasting Tropical Annual Maximum Wet-Bulb Temperatures Months in Advance from the Current State of El Niño
Forecasting Tropical Annual Maximum Wet-Bulb Temperatures Months in Advance from the Current State of El Niño Open
Humid heatwaves, characterized by high temperature and humidity combinations, challenge tropical societies. Extreme wet-bulb temperatures (TW) over tropical land are coupled to the warmest sea surface temperatures (SST) by atmospheric conv…
View article: Non‐Uniqueness in ITCZ Latitude Due To Radiation‐Circulation Coupling in an Idealized GCM
Non‐Uniqueness in ITCZ Latitude Due To Radiation‐Circulation Coupling in an Idealized GCM Open
An idealized aquaplanet moist global atmospheric model with realistic radiative transfer but no clouds and no convective parameterization is found to possess multiple climate equilibria. When forced symmetrically about the equator, in some…
View article: Non-uniqueness in ITCZ latitude due to radiation-circulation coupling in an idealized GCM
Non-uniqueness in ITCZ latitude due to radiation-circulation coupling in an idealized GCM Open
An idealized aquaplanet moist global atmospheric model with realistic radiative transfer but no clouds and no convective parameterization is found to possess multiple climate equilibria: when forced symmetrically about the equator, in some…
View article: Data files for the manuscript "Non-uniqueness in ITCZ latitude due to radiation-circulation coupling in an idealized GCM"
Data files for the manuscript "Non-uniqueness in ITCZ latitude due to radiation-circulation coupling in an idealized GCM" Open
MATLAB scripts and data used to create the figures in the paper "Non-uniqueness in ITCZ latitude due to radiation-circulation coupling in an idealized GCM" by Zurita-Gotor et al., submitted to JAMES.
View article: Data files for the manuscript "Non-uniqueness in ITCZ latitude due to radiation-circulation coupling in an idealized GCM"
Data files for the manuscript "Non-uniqueness in ITCZ latitude due to radiation-circulation coupling in an idealized GCM" Open
MATLAB scripts and data used to create the figures in the paper "Non-uniqueness in ITCZ latitude due to radiation-circulation coupling in an idealized GCM" by Zurita-Gotor et al., submitted to JAMES.
View article: Manabe’s Radiative–Convective Equilibrium
Manabe’s Radiative–Convective Equilibrium Open
Syukoro (Suki) Manabe’s Nobel Prize in Physics was awarded largely for his early work on one-dimensional models of “radiative–convective equilibrium” (RCE), which produced the first credible estimates of Earth’s climate sensitivity. This a…
View article: A Scaling Theory for the Diffusivity of Poleward Eddy Heat Transport Based on Rhines Scaling and the Global Entropy Budget
A Scaling Theory for the Diffusivity of Poleward Eddy Heat Transport Based on Rhines Scaling and the Global Entropy Budget Open
Diffusive theories for the meridional atmospheric energy transport can summarize our understanding of this central aspect of the general circulation. They can also be utilized in simple models of Earth’s energy balance to help interpret th…
View article: Nonlinear generation of long waves and the reversal of eddy momentum fluxes in a two-layer quasi-geostrophic model
Nonlinear generation of long waves and the reversal of eddy momentum fluxes in a two-layer quasi-geostrophic model Open
Although classical theories of midlatitude momentum fluxes focus on the wave-mean flow interaction, wave-wave interactions may be important for generating long waves. It is shown in this study that this nonlinear generation has implication…
View article: Projections of tropical heat stress constrained by atmospheric dynamics
Projections of tropical heat stress constrained by atmospheric dynamics Open
<p>Extreme heat under global warming is a concerning issue for the growing tropical population. However, model projections of extreme temperatures, a widely used metric for extreme heat, are uncertain on regional scales. In addition,…
View article: Projections of tropical heat stress constrained by atmospheric dynamics
Projections of tropical heat stress constrained by atmospheric dynamics Open
View article: NOAA-GFDL GFDL-ESM4 CMIP6 CMIP additional model output
NOAA-GFDL GFDL-ESM4 CMIP6 CMIP additional model output Open
This repository contains annual 3D sea water age since surface contact files from a subset of simulations with GFDL's ESM4.1 climate model (Dunne et al., 2020) that were contributed to the 6th Coupled Model Intercomparison Project (CMIP6).…
View article: NOAA-GFDL GFDL-ESM4 CMIP6 CMIP additional model output
NOAA-GFDL GFDL-ESM4 CMIP6 CMIP additional model output Open
This repository contains annual 3D sea water age since surface contact files from a subset of simulations with GFDL's ESM4.1 climate model (Dunne et al., 2020) that were contributed to the 6th Coupled Model Intercomparison Project (CMIP6).…
View article: NOAA-GFDL GFDL-ESM4 CMIP6 CMIP additional model output
NOAA-GFDL GFDL-ESM4 CMIP6 CMIP additional model output Open
This repository contains annual 3D sea water age since surface contact files from a subset of simulations with GFDL's ESM4.1 climate model (Dunne et al., 2020) that were contributed to the 6th Coupled Model Intercomparison Project (CMIP6).…
View article: The Parameter Dependence of Eddy Heat Flux in a Homogeneous Quasigeostrophic Two-Layer Model on a β Plane with Quadratic Friction
The Parameter Dependence of Eddy Heat Flux in a Homogeneous Quasigeostrophic Two-Layer Model on a β Plane with Quadratic Friction Open
This study investigates the parameter dependence of eddy heat flux in a homogeneous quasigeostrophic two-layer model on a β plane with imposed environmental vertical wind shear and quadratic frictional drag. We examine the extent to which …
View article: Large-scale control on the frequency of tropical cyclones and seeds: a consistent relationship across a hierarchy of global atmospheric models
Large-scale control on the frequency of tropical cyclones and seeds: a consistent relationship across a hierarchy of global atmospheric models Open
A diagnostic framework is developed to explain the response of tropical cyclones (TCs) to climate in high-resolution global atmospheric models having different complexity of boundary conditions. The framework uses vortex dynamics to identi…
View article: The GFDL Earth System Model Version 4.1 (GFDL‐ESM 4.1): Overall Coupled Model Description and Simulation Characteristics
The GFDL Earth System Model Version 4.1 (GFDL‐ESM 4.1): Overall Coupled Model Description and Simulation Characteristics Open
We describe the baseline coupled model configuration and simulation characteristics of GFDL's Earth System Model Version 4.1 (ESM4.1), which builds on component and coupled model developments at GFDL over 2013–2018 for coupled carbon‐chemi…
View article: Using the fast impact of anthropogenic aerosols on regional land temperature to constrain aerosol forcing
Using the fast impact of anthropogenic aerosols on regional land temperature to constrain aerosol forcing Open
Atmospheric simulations of regional land temperature suggest a powerful approach for constraining historical aerosol forcing.
View article: NOAA-GFDL/ESM4: GFDL Earth System Model 4
NOAA-GFDL/ESM4: GFDL Earth System Model 4 Open
This is the public release of ESM4 used for simulations done for publication
View article: Climate Sensitivity of GFDL's CM4.0
Climate Sensitivity of GFDL's CM4.0 Open
GFDL's new CM4.0 climate model has high transient and equilibrium climate sensitivities near the middle of the upper half of CMIP5 models. The CMIP5 models have been criticized for excessive sensitivity based on observations of present‐day…
View article: Structure and Performance of GFDL's CM4.0 Climate Model
Structure and Performance of GFDL's CM4.0 Climate Model Open
We describe the Geophysical Fluid Dynamics Laboratory's CM4.0 physical climate model, with emphasis on those aspects that may be of particular importance to users of this model and its simulations. The model is built with the AM4.0/LM4.0 a…
View article: The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features
The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features Open
We document the configuration and emergent simulation features from the Geophysical Fluid Dynamics Laboratory (GFDL) OM4.0 ocean/sea ice model. OM4 serves as the ocean/sea ice component for the GFDL climate and Earth system models. It is a…
View article: NOAA-GFDL/CM4: CM4.0 Paper Release
NOAA-GFDL/CM4: CM4.0 Paper Release Open
GFDL CM4.0 climate model source code
View article: Aquaplanet Simulations of Tropical Cyclones
Aquaplanet Simulations of Tropical Cyclones Open
View article: Effects of the Mean Flow on Martian Transient Eddy Activity: Studies with an Idealized General Circulation Model
Effects of the Mean Flow on Martian Transient Eddy Activity: Studies with an Idealized General Circulation Model Open
The extent to which the eddy statistics of the Martian atmosphere can be inferred from the mean state and highly simplified assumptions about diabatic and frictional processes is investigated using an idealized general circulation model (G…
View article: The Control of Surface Friction on the Scales of Baroclinic Eddies in a Homogeneous Quasigeostrophic Two-Layer Model
The Control of Surface Friction on the Scales of Baroclinic Eddies in a Homogeneous Quasigeostrophic Two-Layer Model Open
In idealized models of the extratropical troposphere, both β and surface friction can control the equilibrated scales of baroclinic eddies by stopping the inverse cascade. A scaling theory on how surface friction alone sets these scales wa…
View article: The Early Development of the 2015/16 Quasi-Biennial Oscillation Disruption
The Early Development of the 2015/16 Quasi-Biennial Oscillation Disruption Open
An unprecedented disruption of the quasi-biennial oscillation (QBO) started to develop from late 2015. The early development of this event is analyzed using the space–time spectra of eddies from reanalysis data. While the extratropical wav…
View article: 100 Years of Progress in Understanding the General Circulation of the Atmosphere
100 Years of Progress in Understanding the General Circulation of the Atmosphere Open
Some of the advances of the past century in our understanding of the general circulation of the atmosphere are described, starting with a brief summary of some of the key developments from the first half of the twentieth century, but with …
View article: Sensitivity of Radiative‐Convection Equilibrium to Divergence Damping in GFDL‐FV3‐Based Cloud‐Resolving Model Simulations
Sensitivity of Radiative‐Convection Equilibrium to Divergence Damping in GFDL‐FV3‐Based Cloud‐Resolving Model Simulations Open
Using a nonhydrostatic model based on a version of Geophysical Fluid Dynamics Laboratory's FV3 dynamical core at a cloud‐resolving resolution in radiative‐convective equilibrium (RCE) configuration, the sensitivity of the mean RCE climate …