The influence of sea surface temperatures on the northern winter stratosphere : Ensemble simulations with the MAECHAM5 model

By E. Manzini, Marco A. Giorgetta, M. Esch, L. Kornblueh, E. Roeckner. 2006

387 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/509360928bcec6768baae37a61db37a266508a41

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

1. A. Butler
2. C. Garfinkel
3. Adam A. Scaife
4. F. Sassi
5. D. Hartmann
6. A. Charlton-Perez
7. D. Domeisen
8. R. Garcia

In Global and Planetary Change

1. A. Butler
2. C. Garfinkel
3. Adam A. Scaife
4. A. Charlton-Perez
5. F. Sassi
6. D. Domeisen
7. D. Hartmann
8. E. Manzini

Citations in the corpus

• Internal wave coupling processes in Earth's atmosphere (2014, neutral): “…and upper atmosphere models were detached: the former extended only up to the mesosphere (e.g., Boville and Randel , 1992; Beagley et al., 1997; Manzini et al., 2006), while the latter had their lower boundaries at around 80–90 km (e.g., Roble et al., 1988; Richmond et al., 1992); (3) GW…”
• The stratospheric pathway for Arctic impacts on midlatitude climate (2016, background): “…temperature (e.g., 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].”
• Stratospheric Communication of El Niño Teleconnections to European Winter (2009, methodology): “…and tropospheric canonical responses have been reported in other studies, the results of section 3 aim to illustrate the capability of the IGCM in simulating not only the observed spatial and temporal responses, but also the results achieved with more complex GCMs (Manzini et al. 2006).”
• Tropospheric Precursors of Anomalous Northern Hemisphere Stratospheric Polar Vortices (2009, background): “…the shared variance between the AlI and the January and February VSI [VSIresid 5 VSI 2 RAlI,VSIAlI; January and February are the months when Sassi et al. (2004) and Manzini et al. (2006) found a maximum in the ENSO influence on the midstratosphere] and then correlate ENSO with the residual VSI.”
• 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 [In”
• The role of the stratosphere in the European climate response to El Niño (2009, background): “There has been growing observational and modelling evidenc”
• Influence of Tropical Tropopause Layer Cooling on Atlantic Hurricane Activity (2013, background): “…2008; Garcia and Randel 2008; Thompson and Solomon 2009; Fu et al. 2010) and that global climate change may lead to further acceleration of the circulation and associated cooling of the lower tropical stratosphere (Garcia and Randel 2008; Gettelman et al. 2009; McLandress and Shepherd 2009).”
• The predictability of the extratropical stratosphere on monthly time‐scales and its impact on the skill of tropospheric forecasts (2015, background): “(2014) studies showed that planetary wave activity is enhanced and the stratospheric vortex is weaker than normal during the El Niño phase (van Loon and Labitzke, 1987; Sassi et al., 2004; Garcı́a-Herrera et al., 2006; Manzini et al., 2006; Free and Seidel, 2009).”
• Separating the stratospheric and tropospheric pathways of El Niño–Southern Oscillation teleconnections (2013, background): “Similar but oppositely signed anomalies are observed during La Niña winters, albeit with smaller amplitude (Manzini et al 2006, Garfinkel and Hartmann 2007, Free and Seidel 2009).”
• Thermosphere extension of the Whole Atmosphere Community Climate Model (2010, background): “Planetary waves and SSW are also tied to the tropospheric climate system and the stratospheric state, such as the El Niño– Southern Oscillation (ENSO) and quasi‐biennial oscillation (QBO) [e.g., Sassi et al., 2004; Manzini et al., 2006; Holton and Tan, 1980].”
• The Teleconnection of El Niño Southern Oscillation to the Stratosphere (2019, background): “…are however suggested to be offset or superseded in the NH polar regions by the long-term strengthening trend in the BDC (Butchart et al., 2006; Karpechko & Manzini, 2017; Manzini et al., 2014), leading to an overall warming of the Arctic stratosphere and cooling of the lower tropical stratosphere.”
• Tropical rainfall, Rossby waves and regional winter climate predictions (2017, background): “In fact these two factors are also related because ENSO teleconnections have a pathway through the stratosphere (Manzini et al., 2006; Bell et al., 2009) and this again locks the response to winter and amplifies the NAO signature in the extratropics (Ineson and Scaife, 2009).”