Propagation mechanisms for the Madden‐Julian Oscillation

By A. Matthews. 2000

307 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/965e355fe0694db62d0c9f8497eedb799c925653

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. K. Straub
2. Chidong Zhang
3. Á. Adames
4. M. Wheeler
5. G. Kiladis
6. P. Haertel
7. Bin Wang
8. J. Wallace

In Global and Planetary Change

1. K. Straub
2. Chidong Zhang
3. Á. Adames
4. M. Wheeler
5. G. Kiladis
6. P. Haertel
7. Bin Wang
8. J. Wallace

In Oceanography

1. K. Straub
2. Chidong Zhang
3. M. Wheeler
4. Á. Adames
5. J. Wallace
6. B. Hoskins
7. G. Kiladis
8. Miloud Bessafi

Citations in the corpus

• An All-Season Real-Time Multivariate MJO Index: Development of an Index for Monitoring and Prediction (2004, unknown): “…has long been identified through the use of EOF analysis on bandpass-filtered data (e.g., Lau and Chan 1985; Knutson and Weickmann 1987; Maloney and Hartmann 1998; Slingo et al. 1999; Matthews 2000; Kessler 2001), LH00’s use on daily data subject to high-pass filtering only has been relatively unique.”
• MJO Initiation in the Real-Time Multivariate MJO Index (2013, methodology): “Consistent with this finding is the fact that, in the September 1992 primary MJO initiation case study in Matthews (2008), a weak MJO signal is seen in the full RMM index for at least 18 days prior to the OLR-based primary MJO initiation date (not shown).”
• Influence of the Madden–Julian Oscillation on East African rainfall: II. March–May season extremes and interannual variability (2006, unknown): “For instance, Matthews (2000) depicted a ‘cool’ eastward Kelvin wave and a ‘warm’ westward Rossby wave completing a circuit along the equator and meeting 20 days later above West Africa; Hsu and Lee (2005) described this propagation as three consecutive Kelvin waves relaying the signal in the…”
• Propagation and the Vertical Structure of the Madden Julian Oscillation (2003, background): “1996), and more recently as a sea level pressure surge that impacts the Andes and the East African highlands (Matthews 2000).”
• The MJO as a Dispersive, Convectively Coupled Moisture Wave: Theory and Observations (2016, unknown): “5 of Matthews (2000), where it propagates ; 130 8 of longitude from the Maritime Continent to the coast of South America.”
• ENSO regulation of MJO teleconnection (2011, background): “Once the disturbances reach the dateline; thus, over cool equatorial waters, the convection demises and the disturbance is seen only in dynamical fields (Rui and Wang 1990; Hendon and Salby 1994; Matthews 2000; Sperber 2003; Kiladis et al. 2005).”
• Precursor Signals and Processes Associated with MJO Initiation over the Tropical Indian Ocean (2013, background): “…initiation 10 region) related to a previous MJO event that circumnavigates around the global tropics (e.g., Lau 11 and Peng 1987; Wang and Li 1994; Matthews 2000, 2008; Seo and Kim 2003) and processes due 12 to local changes in air-sea fluxes and underlying SST (e.g., Li et al. 2008), planetary…”
• Modulation of South Indian Ocean Tropical Cyclones by the Madden–Julian Oscillation and Convectively Coupled Equatorial Waves (2006, methodology): “5a and 5b) reproduce well those of many previous studies (e.g., Slingo et al. 1999; Lo and Hendon 2000; Matthews 2000), giving confidence that an index developed from the principal component (PC) time series will adequately measure the MJO.”
• The global response to tropical heating in the Madden–Julian oscillation during the northern winter (2004, methodology): “Following Matthews (2000), the MJO life cycle was de ned by an empirical orthogonal function (EOF) analysis of tropical 20{200-day ltered OLR.”
• Zonal and Vertical Structure of the Madden–Julian Oscillation (2005, background): “This rapid phase speed is ascribed to a free first baroclinic Kelvin mode emanating from evolving MJO convection over the warm pool (Milliff and Madden 1996; Hendon and Salby 1996), and it has been argued that the continuation of this signal around the globe is a mechanism for the initiation of the ”
• Madden‐Julian Oscillation (2005, background): “…convective signals of the MJO normally vanish in the eastern Pacific (Figure 2b), its signals in wind and surface pressure continue to propagate farther east as free (uncoupled with convection) waves at much higher speeds of about 30–35 m s 1 [Milliff and Madden, 1996; Matthews, 2000] (Figure 4).”