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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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Clouds, circulation and climate sensitivity

Nature geoscience, 2015-04, Vol.8 (4), p.261-268

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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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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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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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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Clearing clouds of uncertainty

Nature climate change, 2017-10, Vol.7 (10), p.674-678

2017

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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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Tropospheric Adjustment Induces a Cloud Component in CO₂ Forcing

Journal of climate, 2008-01, Vol.21 (1), p.58-71

2008

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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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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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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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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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Local responses to the protection of medieval buildings and archaeology in British post-war town reconstruction: Southampton and Coventry

Urban history, 2018-11, Vol.45 (4), p.635-659

WEBB, MARK S.

2018

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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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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

Clouds, circulation and climate sensitivity

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

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

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

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

Clearing clouds of uncertainty

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

Tropospheric Adjustment Induces a Cloud Component in CO₂ Forcing

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?

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

Prospects for narrowing bounds on Earth's equilibrium climate sensitivity

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

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

Local responses to the protection of medieval buildings and archaeology in British post-war town reconstruction: Southampton and Coventry

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

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