Corpus ID: 14565356

Shortwave and longwave radiative contributions to global warming under increasing CO[subscript 2]

@inproceedings{Donohoe2014ShortwaveAL,
  title={Shortwave and longwave radiative contributions to global warming under increasing CO[subscript 2]},
  author={Aaron Donohoe and Kyle C. Armour and Angeline G. Pendergrass and David S. Battisti},
  year={2014}
}
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References

SHOWING 1-10 OF 47 REFERENCES
Little net clear-sky radiative forcing from recent regional redistribution of aerosols
Aerosols scatter and absorb incoming solar radiation, with consequences for the energy balance of the atmosphere. An analysis of satellite data suggests that the regional redistribution of aerosolsExpand
Observed changes in top-of-the-atmosphere radiation and upper-ocean heating consistent within uncertainty
Global climate change results from a small yet persistent imbalance between the amount of sunlight absorbed by the Earth and the thermal radiation emitted back to space. A revised analysis ofExpand
Tropospheric Adjustment Induces a Cloud Component in CO2 Forcing
Abstract The radiative forcing of CO2 and the climate feedback parameter are evaluated in several climate models with slab oceans by regressing the annual-mean global-mean top-of-atmosphere radiativeExpand
A new method for diagnosing radiative forcing and climate sensitivity
[1] We describe a new method for evaluating the radiative forcing, the climate feedback parameter (W m−2 K−1) and hence the effective climate sensitivity from any GCM experiment in which the climateExpand
Radiative feedbacks on global precipitation
The radiative kernel technique is employed to quantify twenty-first century changes to the tropospheric energy budget in the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment ReportExpand
Radiative forcing by well-mixed greenhouse gases: Estimates from climate models in the Intergovernme
The radiative effects from increased concentrations of well-mixed greenhouse gases (WMGHGs) represent the most significant and best understood anthropogenic forcing of the climate system. The mostExpand
Forcing, feedbacks and climate sensitivity in CMIP5 coupled atmosphere‐ocean climate models
We quantify forcing and feedbacks across available CMIP5 coupled atmosphere-ocean general circulation models (AOGCMs) by analysing simulations forced by an abrupt quadrupling of atmospheric carbonExpand
Thermal expansion of sea water associated with global warming
The relationship between greenhouse-gas forcing, global mean temperature change and sea-level rise due to thermal expansion of the oceans is investigated using upwelling–diffusion and pure diffusionExpand
An observationally based energy balance for the Earth since 1950
[1] We examine the Earth's energy balance since 1950, identifying results that can be obtained without using global climate models. Important terms that can be constrained using only measurements andExpand
An Assessment of Climate Feedbacks in Coupled Ocean–Atmosphere Models
Abstract The climate feedbacks in coupled ocean–atmosphere models are compared using a coordinated set of twenty-first-century climate change experiments. Water vapor is found to provide the largestExpand
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4
5
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