The Growth and Triggering Mechanisms of the PNA : A MJO-PNA Coherence

By M. Mori, Masahiro Watanabe. 2008

207 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/b083a61a5e5bb8cd26dae980644eb800aeeacf0a

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Citations in the corpus

ENSO regulation of MJO teleconnection (2011, background): “…the notion that the change of position in the anomalous tropical convection can induce a large difference over the extratropical flow (Branstator 2003) and the notion that the Pacific-North American sector is sensitive to the tropical Pacific SST (Hoering and Kumar 2002; Mori and Watanabe 2008).”
Review of Tropical‐Extratropical Teleconnections on Intraseasonal Time Scales (2017, methodology): “The dynamical link between MJO and PNA suggested by analysis of observations was tested by Mori and Watanabe (2008) in forced numerical experiments with a linear barotropic model.”
Fifty Years of Research on the Madden‐Julian Oscillation: Recent Progress, Challenges, and Perspectives (2020, background): “M. Mori and Watanabe (2008) found that the development of the PNA can be triggered by the MJO convection activity in the tropical Indian Ocean and western Pacific.”
Low‐frequency nonlinearity and regime behavior in the Northern Hemisphere extratropical atmosphere (2017, background): “…2014] and are stabilized by local midlatitude processes such as transient eddy vorticity fluxes or diabatic heating [Mitchell and Derome, 1983; Shutts, 1987; Marshall and So, 1990; Adames and Wallace, 2014; Lau et al., 2012; Lin et al., 2009; Mori and Watanabe, 2008; Molteni et al., 2011].”
Three-Dimensional Structure and Evolution of the MJO and Its Relation to the Mean Flow (2014, background): “…to tropical forcing: specifically the advection of planetary vorticity by the divergent, upper-tropospheric outflow from the enhanced convection as proposed by Sardeshmukh and Hoskins (1988); for example, see Matthews et al. (2004), Mori and Watanabe (2008), and Frederiksen and Lin (2013).”
The impact of the MJO on clusters of wintertime circulation anomalies over the North American region (2012, background): “Consistent with this basic mechanism, observational studies have found that the positive (negative) phase of the PNA is more common during and after MJO-related enhanced (suppressed) convection over the western and central tropical Pacific (e.g, Ferranti et al. 1990; Higgins and Mo 1997; Johnson and”