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The Dependence of Global Cloud and Lapse Rate Feedbacks on the Spatial Structure of Tropical Pacific Warming

Journal of climate, 2018-01, Vol.31 (2), p.641-654

2018

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The Dependence of Radiative Forcing and Feedback on Evolving Patterns of Surface Temperature Change in Climate Models

Journal of climate, 2015-02, Vol.28 (4), p.1630-1648

2015

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Forcing, feedbacks and climate sensitivity in CMIP5 coupled atmosphere-ocean climate models

Geophysical research letters, 2012-05, Vol.39 (9), p.n/a

2012

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Mechanisms of the Negative Shortwave Cloud Feedback in Middle to High Latitudes

Journal of climate, 2016-01, Vol.29 (1), p.139-157

2016

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Contributions of Different Cloud Types to Feedbacks and Rapid Adjustments in CMIP5

Journal of climate, 2013-07, Vol.26 (14), p.5007-5027

2013

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Accounting for Changing Temperature Patterns Increases Historical Estimates of Climate Sensitivity

Geophysical research letters, 2018-08, Vol.45 (16), p.8490-8499

2018

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Positive Low Cloud Feedback Primarily Caused by Increasing Longwave Radiation From the Sea Surface in Two Versions of a Climate Model

Geophysical research letters, 2023-10, Vol.50 (20), p.n/a

2023

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Global-mean radiative feedbacks and forcing in atmosphere-only and coupled atmosphere-ocean climate change experiments

Geophysical research letters, 2014-06, Vol.41 (11), p.4035-4042

2014

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Origins of differences in climate sensitivity, forcing and feedback in climate models

Climate dynamics, 2013-02, Vol.40 (3-4), p.677-707

2013

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Coupling between subtropical cloud feedback and the local hydrological cycle in a climate model

Climate dynamics, 2013-10, Vol.41 (7-8), p.1923-1939

2013

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The Cloud Feedback Model Intercomparison Project (CFMIP) contribution to CMIP6

Geoscientific Model Development, 2017-01, Vol.10 (1), p.359-384

2017

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Fixed Anvil Temperature Feedback: Positive, Zero, or Negative?

Journal of climate, 2020-04, Vol.33 (7), p.2719-2739

2020

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The Impact of Parameterized Convection on Climatological Precipitation in Atmospheric Global Climate Models

Geophysical research letters, 2018-04, Vol.45 (8), p.3728-3736

2018

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Multivariate probabilistic projections using imperfect climate models part I: outline of methodology

Climate dynamics, 2012-06, Vol.38 (11-12), p.2513-2542

2012

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Projected increase in continental runoff due to plant responses to increasing carbon dioxide

Nature (London), 2007-08, Vol.448 (7157), p.1037-1041

2007

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What Are the Main Causes of Positive Subtropical Low Cloud Feedbacks in Climate Models?

Journal of advances in modeling earth systems, 2024-01, Vol.16 (1), p.n/a

2024

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Prospects for narrowing bounds on Earth's equilibrium climate sensitivity

Earth's future, 2016-11, Vol.4 (11), p.512-522

2016

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Climate model errors, feedbacks and forcings: a comparison of perturbed physics and multi-model ensembles

Climate dynamics, 2011-05, Vol.36 (9-10), p.1737-1766

2011

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Mechanisms for the land/sea warming contrast exhibited by simulations of climate change

Climate dynamics, 2008-04, Vol.30 (5), p.455-465

2008

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The Relationship between Land–Ocean Surface Temperature Contrast and Radiative Forcing

Journal of climate, 2011-07, Vol.24 (13), p.3239-3256

2011

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Interactions between Hydrological Sensitivity, Radiative Cooling, Stability, and Low-Level Cloud Amount Feedback

Journal of climate, 2018-03, Vol.31 (5), p.1833-1850

2018

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Regional Intensification of the Tropical Hydrological Cycle During ENSO

Geophysical research letters, 2018-05, Vol.45 (9), p.4361-4370

2018

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The impact of parametrized convection on cloud feedback

Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences, 2015-11, Vol.373 (2054), p.20140414

2015

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Testing a Physical Hypothesis for the Relationship Between Climate Sensitivity and Double‐ITCZ Bias in Climate Models

Journal of advances in modeling earth systems, 2020-09, Vol.12 (9), p.n/a

2020

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Robustness, uncertainties, and emergent constraints in the radiative responses of stratocumulus cloud regimes to future warming

Climate dynamics, 2016-05, Vol.46 (9-10), p.3025-3039

2016

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The Dependence of Global Cloud and Lapse Rate Feedbacks on the Spatial Structure of Tropical Pacific Warming

The Dependence of Radiative Forcing and Feedback on Evolving Patterns of Surface Temperature Change in Climate Models

Forcing, feedbacks and climate sensitivity in CMIP5 coupled atmosphere-ocean climate models

Mechanisms of the Negative Shortwave Cloud Feedback in Middle to High Latitudes

Contributions of Different Cloud Types to Feedbacks and Rapid Adjustments in CMIP5

Accounting for Changing Temperature Patterns Increases Historical Estimates of Climate Sensitivity

Positive Low Cloud Feedback Primarily Caused by Increasing Longwave Radiation From the Sea Surface in Two Versions of a Climate Model

Global-mean radiative feedbacks and forcing in atmosphere-only and coupled atmosphere-ocean climate change experiments

Origins of differences in climate sensitivity, forcing and feedback in climate models

Coupling between subtropical cloud feedback and the local hydrological cycle in a climate model

The Cloud Feedback Model Intercomparison Project (CFMIP) contribution to CMIP6

Fixed Anvil Temperature Feedback: Positive, Zero, or Negative?

The Impact of Parameterized Convection on Climatological Precipitation in Atmospheric Global Climate Models

Multivariate probabilistic projections using imperfect climate models part I: outline of methodology

Projected increase in continental runoff due to plant responses to increasing carbon dioxide

What Are the Main Causes of Positive Subtropical Low Cloud Feedbacks in Climate Models?

Prospects for narrowing bounds on Earth's equilibrium climate sensitivity

Climate model errors, feedbacks and forcings: a comparison of perturbed physics and multi-model ensembles

Mechanisms for the land/sea warming contrast exhibited by simulations of climate change

The Relationship between Land–Ocean Surface Temperature Contrast and Radiative Forcing

Interactions between Hydrological Sensitivity, Radiative Cooling, Stability, and Low-Level Cloud Amount Feedback

Regional Intensification of the Tropical Hydrological Cycle During ENSO

The impact of parametrized convection on cloud feedback

Testing a Physical Hypothesis for the Relationship Between Climate Sensitivity and Double‐ITCZ Bias in Climate Models

Robustness, uncertainties, and emergent constraints in the radiative responses of stratocumulus cloud regimes to future warming

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