Polar amplification in a coupled climate model with locked albedo
By Rune Graversen, Minghuai Wang. 2009
335 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/3b893333adcb6629a5d48e026a1a0fd5e9aca5d0
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In Atmospheric Science
In Global and Planetary Change
Citations in the corpus
- Coupling between Arctic feedbacks and changes in poleward energy transport (2011, background): “In terms of energy transport, increasing moisture transport in a warmer climate was found to be responsible for enhanced Arctic warming in idealized experiments without surface albedo feedback [Hall, 2004; Alexeev et al., 2005; Graversen and Wang, 2009].”
- Extreme moisture transport into the Arctic linked to Rossby wave breaking (2014, background): “Although a surface albedo feedback may play a role in this amplified warming [e.g., Manabe and Wetherald, 1975; Manabe and Stouffer, 1980], some studies also highlight longwave radiation as another potential culprit [e.g., Winton, 2006; Graversen and Wang, 2009].”
- Evolution of the Global Coupled Climate Response to Arctic Sea Ice Loss during 1990–2090 and Its Contribution to Climate Change (2018, background): “…response to Arctic sea ice loss, either by altering the sea ice parameters such as albedo (e.g., Bitz et al. 2006; Winton 2008; Scinocca et al. 2009; Graversen and Wang 2009; Blackport and Kushner 2016, 2017; Cvijanovic et al. 2017) or by adding an additional heat flux to the sea ice throughout…”
- Mechanisms of summertime upper Arctic Ocean warming and the effect on sea ice melt (2010, methodology): “" Several papers discuss how to quantify this feedback [e.g., Graversen and Wang, 2009; Winton, 2006], for example by defining an amplification factor and then running twin experiments with fully coupled models, a control experiment and another with a " locked " climatological daily average albedo.”
- Arctic amplification of climate change: a review of underlying mechanisms (2021, background): “…when effects on the PET are also taken into account (such as in ‘feedback-locking’ experiments with climate models; e.g. Vavrus 2004, Graversen and Wang 2009, Graversen et al 2014, Merlis 2014, Ceppi and Hartmann 2016, Dai et al 2019, Dekker et al 2019, Li and Newman 2020, Middlemas et al…”
- Polar Amplification in CCSM4: Contributions from the Lapse Rate and Surface Albedo Feedbacks (2014, methodology): “…wherein feedbacks are suppressed in climate models has been applied earlier in order to study the surface albedo feedback (Hall 2004; Graversen and Wang 2009; Mauritsen et al. 2013), the water vapor feedback (Schneider et al. 1999; Hall and Manabe 1999; Langen et al. 2012; Mauritsen et al. 2013),…”
- The Polar Amplification Model Intercomparison Project (PAMIP) contribution to CMIP6: investigating the causes and consequences of polar amplification (2018, neutral): “Other feedbacks are also potentially important in controlling temperature trends in polar regions, including water vapour (Graversen and Wang, 2009) and clouds (Vavrus, 2004), and changes in heat transport in the atmosphere (Manabe and Wetherald, 1980) and ocean (Khodri et al.”