Importance of the mixed-phase cloud distribution in the control climate for assessing the response of clouds to carbon dioxide increase: a multi-model study
By Y. Tsushima, S. Emori, T. Ogura, M. Kimoto, Mark J. Webb, K. Williams, M. Ringer, Brian J. Soden, B. Li, N. Andronova. 2006
197 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/a687162c83624d0cf687546dc58af3e60d2b8577
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In Global and Planetary Change
Citations in the corpus
- Mixed‐phase cloud physics and Southern Ocean cloud feedback in climate models (2015, background): “This is consistent with liquid clouds thinning for the reasons that we discussed earlier [Bretherton et al., 2013; Tsushima et al., 2006].”
- Contributions of Different Cloud Types to Feedbacks and Rapid Adjustments in CMIP5 (2012, background): “…for cloudmasking increases net cloud feedback by 0.3 W m22 K21, whereas accounting for rapid adjustments reduces by 0.14 W m22 K21 the ensemble mean net cloud feedback through a combination of smaller positive cloud amount and altitude feedbacks and larger negative optical depth feedbacks.”
- Computing and Partitioning Cloud Feedbacks Using Cloud Property Histograms. Part II: Attribution to Changes in Cloud Amount, Altitude, and Optical Depth (2012, background): “, Weaver (2003); Vavrus et al. (2009); Wu et al. (2010)) to cloud fraction 356 increases associated with the poleward-shifted storm track (Hall et al.”
- Cloud feedback mechanisms and their representation in global climate models (2017, unknown): “We refer the reader to Andrews et al. 43 and Kamae et al. 44 for a thorough discussion of rapid cloud adjustments in GCMs.”
- Emergent Constraints for Cloud Feedbacks (2015, unknown): “Other factors, such as the change from ice or mixed-phase cloud to more liquid dominant clouds [44], may contribute to intermodel spread and the models’ positive bias with respect to observations.”
- Insights from a refined decomposition of cloud feedbacks (2016, background): “…the region of persistent mixed phase clouds over the Southern Ocean, likely due to warming-induced transitions from ice- to liquid-dominated clouds [Tsushima et al., 2006; McCoy et al., 2015; Tan et al., 2016; Ceppi et al., 2016a] and increases in adiabatic water content, which are more pronounced…”
- Connections Between Clouds, Radiation, and Midlatitude Dynamics: a Review (2015, background): “Around the midlatitudes, changes in optical depth associated with the amount of cloud liquid water appear to be particularly relevant to the cloud feedback, driven by the SW effect of low clouds [27, 31, 32, 39, 40].”