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Global warming due to increasing absorbed solar radiation

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Global warming due to increasing absorbed solar radiation (English)

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Kevin E. Trenberth

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John T. Fasullo

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John T. Fasullo

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English

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publication date

14 April 2009

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published in

Geophysical Research Letters

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volume

36

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issue

7

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cites work

Marine boundary layer clouds at the heart of tropical cloud feedback uncertainties in climate models

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On dynamic and thermodynamic components of cloud changes

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How Well Do We Understand and Evaluate Climate Change Feedback Processes?

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Improved estimates of upper-ocean warming and multi-decadal sea-level rise.

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The Annual Cycle of the Energy Budget. Part I: Global Mean and Land–Ocean Exchanges

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The Annual Cycle of the Energy Budget. Part II: Meridional Structures and Poleward Transports

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21 January 2018

Aquaplanets, Climate Sensitivity, and Low Clouds

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An Assessment of Climate Feedbacks in Coupled Ocean–Atmosphere Models

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21 January 2018

Recent Trends in Cloudiness over the United States: A Tale of Monitoring Inadequacies

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Cumulus Microphysics and Climate Sensitivity

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CloudSat mission: Performance and early science after the first year of operation

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Trends in Global Cloud Cover in Two Decades of HIRS Observations

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A comparison of low-latitude cloud properties and their response to climate change in three AGCMs sorted into regimes using mid-tropospheric vertical velocity

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The Seasonal Cycle of Low Stratiform Clouds

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The Iris Hypothesis: A Negative or Positive Cloud Feedback?

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Does the Earth Have an Adaptive Infrared Iris?

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Widening of the tropical belt in a changing climate

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Global warming due to increasing absorbed solar radiation

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