The role of the stratosphere in the European climate response to El Niño

By S. Ineson, Adam A. Scaife. 2009

496 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/603e985056e19da2252ded81dbde51d6d3abff58

How researchers see this paper

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

In Atmospheric Science

In Global and Planetary Change

Citations in the corpus

Seasonal winter forecasts and the stratosphere (2016, background): “…Hartmann, 2006; Bell et al., 2009; Butler and Polvani, 2011; Domeisen et al., 2015) and the need for this stratospheric response in order to generate a strong surface NAO signal in the Atlantic (Toniazzo and Scaife, 2006; Cagnazzo and Manzini, 2009; Ineson and Scaife, 2009; Butler et al., 2014).”
The predictability of the extratropical stratosphere on monthly time‐scales and its impact on the skill of tropospheric forecasts (2015, methodology): “In the following sections, we group experiments by type and summarize their collective results.”
The Role of Linear Interference in the Annular Mode Response to Tropical SST Forcing (2010, background): “closely resembles the response found in other models (Ineson and Scaife 2009; Cagnazzo and Manzini 2009) and the NAM pattern that is coherent with El Niño in observations (Garfinkel and Hartmann 2008).”
Impact of the QBO on surface winter climate (2009, background): “General circulation model simulations that reproduce the observed response have recently identified a link between ENSO and the northern polar vortex via the stratosphere [Manzini et al., 2006] and shown a European surface NAO response that is large enough to be useful for seasonal forecasting [ Ine”
Tropospheric Precursors of Anomalous Northern Hemisphere Stratospheric Polar Vortices (2009, background): “Ineson and Scaife (2009) find that this pathway is important for ENSO’s effect on European climate.”
Stratospheric Communication of El Niño Teleconnections to European Winter (2009, background): “Recently, it has also been demonstrated that the frequency modulation of SSW events plays an important role in the late winter MSLP signal, such that the modeled canonical response is only simulated in winters with a dynamically active stratosphere (Ineson and Scaife 2009).”
Observed connection between stratospheric sudden warmings and the Madden‐Julian Oscillation (2012, unknown): “…during an El Niño winter, mid-tropospheric geopotential heights are anomalously low in the NP, and these teleconnections with the midlatitudes have been linked with a weakened polar vortex [ Garfinkel and Hartmann , 2008; Bell et al. , 2009; Ineson and Scaife , 2009; Garfinkel et al. , 2010, 2012].”
The Role of the Stratosphere in Subseasonal to Seasonal Prediction: 2. Predictability Arising From Stratosphere‐Troposphere Coupling (2020, background): “…is, by El Niño–Southern Oscillation (ENSO) (Butler et al., 2014, 2016; Butler & Polvani, 2011; Domeisen et al., 2015; Garfinkel & Hartmann, 2007; Ineson & Scaife, 2009; Manzini et al., 2006; Polvani et al., 2017; Song & Son, 2018), for a summary see Domeisen et al. (2019), tropical convection…”
Assessing and understanding the impact of stratospheric dynamics and variability on the earth system (2012, background): “The vortex anomalies then propagate downward, affecting the midlatitudes in the troposphere (Cagnazzo and Manzini 2009; Ineson and Scaife 2009).”
The stratospheric pathway for Arctic impacts on midlatitude climate (2016, background): “, El Niño– Southern Oscillation), ozone, and greenhouse gases, that can affect the stratospheric polar vortex strength with consequential downward influences on the surface climate [Brönnimann et al., 2004; Manzini et al., 2006; Ineson and Scaife, 2009; Kidston et al., 2015].”
Impact of ENSO on the Atmospheric Variability over the North Atlantic in Late Winter—Role of Transient Eddies (2012, background): “2004, 2007) and numerical experimentation (Merkel and Latif 2002; Gouirand et al. 2007; Ineson and Scaife 2009) indicate that ENSO can extend its influence to the remote North Atlantic– European sector, with responses in early winter being different from those in late winter.”
Tropospheric Precursors and Stratospheric Warmings (2011, background): “Other observational and modeling studies have confirmed that tropospheric precursors to stratospheric warmings can be associated with Eurasian snow cover variability, the El Niño– Southern Oscillation, and atmospheric blocking.”
SEAS5: the new ECMWF seasonal forecast system (2018, background): “Teleconnections from the tropical oceans to the mid-latitudes may be mediated by the stratosphere (Bell et al., 2009; Ineson and Scaife, 2009), placing importance on correctly representing the mean stratosphere climate (Maycock et al.”
Defining Sudden Stratospheric Warmings (2015, background): “…of tropospheric CO2 and pollutants (Jiang et al. 2013), the extension of the El Niño–Southern Oscillation (ENSO) teleconnection into Eurasia (e.g., Ineson and Scaife 2009; Butler et al. 2014b), decadal variability in the North Atlantic Ocean circulation (Reichler 1 Stratospheric sudden warming…”
Separating the stratospheric and tropospheric pathways of El Niño–Southern Oscillation teleconnections (2013, methodology): “First, calculations for SSW central dates using the current version of NCEP-NCAR reanalysis no longer detect a SSW in January 1968, which also appeared in the table of Charlton and Polvani (2007); this is likely due to slight differences in versions of the data.”