Intraseasonal interaction between the Madden–Julian Oscillation and the North Atlantic Oscillation

By C. Cassou. Nature, 2008

772 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/05e60ab3a03a3b5f6acb547945aa2055f44f88cb

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In Atmospheric Science

1. F. Vitart
2. Chidong Zhang
3. E. Maloney
4. K. Straub
5. A. Butler
6. Á. Adames
7. T. Woollings
8. Hai Lin

In Global and Planetary Change

1. F. Vitart
2. Chidong Zhang
3. E. Maloney
4. Á. Adames
5. K. Straub
6. A. Butler
7. C. DeMott
8. N. Klingaman

Citations in the corpus

• ENSO regulation of MJO teleconnection (2011, background): “In the lower-level, a pair of cyclonic anomalies is nearly 180 out of phase with the corresponding upper-level anticyclones, which dissipate after reaching the central Pacific, although the upper tropospheric anomalies continue to traverse the Western Hemisphere (Lorenc 1984; Knutson et al. 1986; Ru”
• MJO Initiation in the Real-Time Multivariate MJO Index (2013, background): “…into upcoming flood, drought, tropical cyclogenesis, and high-amplitude extratropical weather probabilities (e.g., Higgins et al. 2000; Jones 2000; Maloney and Hartmann 2000; Hall et al. 2001; Bond andVecchi 2003; Bessafi and Wheeler 2006; Cassou 2008; Lin and Brunet 2009; Jones et al. 2011).”
• The influence of weather regimes on European renewable energy production and demand (2019, methodology): “These patterns match similar classifications in earlier research (e.g. Vautard 1990, Michelangeli et al 1995, Cassou 2008).”
• Seasonal climate forecasting (2010, background): “Cassou (2008) provided a clear example of such interaction, demonstrating a clear link between the MJO and the regimes in the North Atlantic European region.”
• Variability of the North Atlantic eddy‐driven jet stream (2010, positive): “In some of these studies the agreement with the three anomaly patterns in Figure 4 is strong ( e.g. Cassou 2008).”
• The Met Office Global Coupled Model 3.0 and 3.1 (GC3.0 and GC3.1) Configurations (2017, background): “In addition to being a direct source of precipitation variability for regions such as the Maritime Continent and northern Australia, teleconnections from the MJO have been shown to affect other parts of the tropics and variability in the midlatitudes (e.g., Cassou, 2008).”
• The impact of the MJO on clusters of wintertime circulation anomalies over the North American region (2012, methodology): “Consistent with previous results (e.g., Cassou 2008; L’Heureux and Higgins 2008; and Lin et al. 2009), Cluster 4 probabilities are elevated approximately 10-20 days after an MJO event in phase 7.”
• The Link between Rossby Wave Breakings and Weather Regime Transitions (2011, background): “GA and Z streamfunction anomalies strongly project onto the negative and positive phases of the NAO, respectively, and are often referred to them in the literature (e.g., Cassou 2008).”
• Heatwave classification over Europe and the Mediterranean region (2012, background): “Cassou et al (2005) and Cassou (2008) investigated the influence of tropical oceans on weather patterns in the North Atlantic.”
• Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, background): “Similar results of the association between the MJO and NAO were reported in Cassou (2008).”
• MJO simulation in CMIP5 climate models: MJO skill metrics and process-oriented diagnosis (2017, neutral): “…(Weickmann et al. 1985; Ferranti et al. 1990; Berbery and Nogués-Paegle 1993; Higgins and Mo 1997; Matthews et al. 2004; Vecchi and Bond 2004; Cassou 2008; L’Heureux and Higgins 2008; Lin et al. 2009; Johnson and Feldstein 2010; Seo and Son 2011; Garfinkel et al. 2012; Guan et al. 2012; Yoo…”
• Analysis of daily river flow fluctuations using Empirical Mode Decomposition and arbitrary order Hilbert spectral analysis (2009, background): “The latter may be288 linked to the Madden-Julian Oscillation (MJO), since some connection be-289 tween and the North Atlantic Oscillation (NAO) and MJO have been found290 (Cassou, 2008).”
• SEAS5: the new ECMWF seasonal forecast system (2018, background): “Since links between Indian Ocean rainfall and the NAO are also evident on the sub-seasonal time scale (Cassou, 2008; 10 Lin et al., 2009), future analysis of SEAS5 performance in reproducing tropical intra-seasonal variability (such as the Madden-”
• Propagation of the Madden–Julian Oscillation through the Maritime Continent and scale interaction with the diurnal cycle of precipitation (2014, background): “…other tropical weather features, such as tropical cyclones (e.g. Camargo et al., 2009), including hurricanes in the Gulf of Mexico (Maloney and Hartmann, 2000), and ENSO (e.g. Hendon et al., 2007); it also affects extratropical weather through teleconnections (e.g. Kim et al., 2006; Cassou, 2008).”
• Atmosphere‐ocean coupled processes in the Madden‐Julian oscillation (2015, background): “, 2000], which play an important role in western North American water supplies but are also linked to floods and landslides; interactions with the polar Southern [Matthews and Meredith, 2004] and Northern Annular Modes and cold air outbreaks over Europe [Zhou and Miller, 2005; Cassou, 2008; Lin et a”
• Forcing of the wintertime atmospheric circulation by the multidecadal fluctuations of the North Atlantic ocean (2014, methodology): “They are: the blocking regime, the Atlantic Ridge regime, the positive NAO regime (NAO+, also called the Atlantic low regime) and the negative NAO regime (NAO−) (Cassou 2008).”
• The predictability of the extratropical stratosphere on monthly time‐scales and its impact on the skill of tropospheric forecasts (2015, background): “Cassou (2008) shows this coupling as an asymmetric tropical–extratropical lagged relationship with the North Atlantic Oscillation (NAO) where MJO preconditioning occurs for positive (negative) NAO events as a midlatitude wave train initiated by the MJO in the western-central tropical Pacific (easter”
• The Teleconnection of El Niño Southern Oscillation to the Stratosphere (2019, background): “…be used to consider possible nonlinearities of the stratospheric response to wave trains from the tropics in a far-larger sample than is currently possible with ENSO (e.g., Cassou, 2008; Garfinkel, Feldstein, et al., 2012; Kang & Tziperman, 2017; Scaife et al., 2017; Schwartz & Garfinkel, 2017).”