CMIP5 multimodel ensemble projection of storm track change under global warming
By E. Chang, Yanjuan Guo, X. Xia. 2012
355 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/edd47fa04072cb169dc233b0af512de6a9194ec8
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In Atmospheric Science
- Andrew Gettelman
- Richard B. Neale
- J. Richter
- R. Garcia
- D. Hartmann
- D. Marsh
- P. Ceppi
- Peter H. Lauritzen
In Global and Planetary Change
- Andrew Gettelman
- Richard B. Neale
- P. Ceppi
- D. Hartmann
- J. Richter
- R. Garcia
- Peter H. Lauritzen
- D. Marsh
Citations in the corpus
- Connections Between Clouds, Radiation, and Midlatitude Dynamics: a Review (2015, background): “However, projected storminess changes in CMIP5 are robustly positive only in the SH [35].”
- Extreme Precipitation Indices over China in CMIP5 Models. Part II: Probabilistic Projection (2016, background): “…of climate change in the future (Sillmann et al. 2013; Kharin et al. 2013; Thibeault and Seth 2014; Swain and Hayhoe 2015), because an MME can reduce the uncertainties and increase the reliability of prediction (Shongwe et al. 2009; Chang et al. 2012; Gao et al. 2012; Villarini and Vecchi 2012).”
- Extreme cyclone events in the Arctic: Wintertime variability and trends (2017, methodology): “Previous studies on extreme Arctic cyclones have focused almost exclusively on the annual or seasonal means [Sepp and Jaagus 2011, Chang et al 2012, Vavrus 2013].”
- An Evaluation of the Large‐Scale Atmospheric Circulation and Its Variability in CESM2 and Other CMIP Models (2020, methodology): “…jet stream that is too far south during the winter (Barnes & Polvani, 2013; Delcambre et al., 2013; Woollings & Blackburn, 2011) and a general tendency toward storm tracks that are too weak in summer and winter, both in terms of cyclone number and intensity (Chang et al., 2012; Zappa et al., 2013).”
- A Diagnosis of the Seasonally and Longitudinally Varying Midlatitude Circulation Response to Global Warming (2014, background): “…anomalies onto the dominant modes of variability (e.g., the northern or southern annular modes) (e.g., Miller et al. 2006; Previdi and Liepert 2007; Woollings and Blackburn 2012; Gillett and Fyfe 2013), or 3) trends in diagnostics related to storm-track activity (e.g., Yin 2005; Chang et al. 2012).”