Variability of the North Atlantic eddy‐driven jet stream

589 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

The Met Office Global Coupled Model 3.0 and 3.1 (GC3.0 and GC3.1) Configurations (2017, background): “frequency distribution being present in the winter and a skewed structure in the summer (Figure 15; Woollings et al., 2010).”
Extreme moisture transport into the Arctic linked to Rossby wave breaking (2014, background): “The level of 850 hPa is chosen to capture the eddy-driven part of the jet stream [e.g., Barnes and Hartmann, 2010; Woollings et al., 2010].”
An Evaluation of the Large‐Scale Atmospheric Circulation and Its Variability in CESM2 and Other CMIP Models (2020, background): “As demonstrated by Woollings et al. (2010), the climatology of the North Atlantic jet stream in winter is really the average over three preferred states.”
Blocking and its Response to Climate Change (2018, background): “This approach captures classical mid-latitude blocks associated with the weakening of the jet stream, but also high-latitude and low-latitude blocks, which rather involve southward and northward shifts of the jet stream respectively [94, 95].”