Climate Feedbacks and Their Implications for Poleward Energy Flux Changes in a Warming Climate
By M. Zelinka, D. Hartmann. 2011
139 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/e9101f5d30ebe699aaec2dfce2dc9a0a1e993b58
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Citations in the corpus
- Computing and Partitioning Cloud Feedbacks Using Cloud Property Histograms. Part II: Attribution to Changes in Cloud Amount, Altitude, and Optical Depth (2012, background): “Nevertheless, the tendency for tropical clouds to systematically rise as the planet warms is consistent with theory [i.e., the fixed anvil temperature hypothesis of Hartmann and Larson (2002)], cloud-resolving model experiments (Tompkins and Craig 1999; Kuang and Hartmann 2007; Harrop and Hartmann 2”
- The dependence of transient climate sensitivity and radiative feedbacks on the spatial pattern of ocean heat uptake (2014, background): “SW cloud feedback is negative193 at high latitudes in all cases, attributable to an increase in optical thickness of cold clouds194 with temperature [Zelinka and Hartmann, 2012].195 To summarize, our different forcing scenarios excite different feedback patterns, domi-196 nated by SW cloud effects.”
- Time-Varying Climate Sensitivity from Regional Feedbacks (2012, background): “Within models, estimates of climate feedbacks based on transient warming scenarios (e.g., Soden and Held 2006; Zelinka and Hartmann 2011) can be expected to produce different spatial effective feedback patterns, and a different global effective feedback, than those estimates based on equilibrium sce”
- Arctic amplification of climate change: a review of underlying mechanisms (2021, background): “In accordance with this, coupled climate models forced with increased CO2 robustly simulate increases in atmospheric PET in the midlatitudes of both hemispheres (Held and Soden 2006, Hwang and Frierson 2010, Wu et al 2011, Zelinka and Hartmann 2012, Huang and Zhang 2014, Armour et al 2019).”
- The Surface Downwelling Solar Radiation Surplus over the Southern Ocean in the Met Office Model: The Role of Midlatitude Cyclone Clouds (2012, unknown): “(Zelinka and Hartmann 2012).”
- Extratropical Cooling, Interhemispheric Thermal Gradients, and Tropical Climate Change (2012, background): “Another study by Zelinka & Hartmann (2012) identified the Southern Ocean as a possible source of relative cooling because of the strong heat absorption there, necessitating interhemispheric energy fluxes that shift the ITCZ.”