The Global Atmospheric Circulation Response to Tropical Diabatic Heating Associated with the Madden–Julian Oscillation during Northern Winter
175 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/e5d60985859d3a94dd4c1550019c6b7a6620f38f
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Citations in the corpus
- MJO simulation in CMIP5 climate models: MJO skill metrics and process-oriented diagnosis (2017, unknown): “…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 et al. 2012; Henderson et al. 2016; Mundhenk et al. 2016).”
- Stratospheric control of the Madden-Julian oscillation. (2017, methodology): “Because the longitudinal distribution of the tropical tropopause temperature is largely determined by the underlying convection (Kim and Son 2012), its spatial pattern follows the DJF-mean OLR distribution very well (cf. Fig.”
- A Comparison of OLR and Circulation-Based Indices for Tracking the MJO (2014, background): “…once established, the convective component provides the critical link to the instability mechanism of the disturbance (Raymond and Fuchs 2009; Khouider et al. 2012; Liu Unauthenticated | Downloaded 03/27/22 04:52 AM UTC and Wang 2012) and its teleconnections (Seo and Song 2012; Dole et al. 2014).”
- The East Atlantic/West Russia (EA/WR) teleconnection in the North Atlantic: climate impact and relation to Rossby wave propagation (2015, background): “Sardeshmukh and Hoskins (1988) and Qin and Robinson (1993) found that the first and fourth terms capture the main features of the tropical source whereas the second and third terms determine the main features of the extratropical RWS (Seo and Son 2012).”
- Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, background): “The general features of extratropical atmospheric response to the MJO can be simulated using simple numerical models with idealized tropical thermal forcing (e.g., H. Lin et al., 2010; Matthews et al., 2004; K. H. Seo & Son, 2012; K.‐C. Tseng et al., 2019).”
- Three-Dimensional Structure and Evolution of the MJO and Its Relation to the Mean Flow (2014, background): “10c), the MJO-related easterly anomalies along 328N at the date line overlie the climatological-mean jet exit region and are thereby capable of extracting kinetic energy from themean flow, as described in Simmons et al. (1983) and Nakamura et al. (1987).”
- Review of Tropical‐Extratropical Teleconnections on Intraseasonal Time Scales (2017, background): “Subseasonal Cariations of Precipitation and Near-Surface Air Temperature The MJO is associated with modulation of temperature and precipitation on a global basis (e.g., Donald et al., 2006; Hoell et al., 2013; Matsueda & Takaya, 2015; Seo & Son, 2012), including extreme events.”