Primary and successive events in the Madden–Julian Oscillation
By A. Matthews. 2008
237 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/cf735e6cc791067340713fdfeb858be8d84dd762
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
In Global and Planetary Change
In Oceanography
Citations in the corpus
- Multiscale Convective Organization and the YOTC Virtual Global Field Campaign (2012, background): “1181august 2012aMERICaN MEtEOROLOgICaL sOCIEtY | • The MJO tends to regenerate more frequently from a previous MJO than observations (e.g., Matthews 2007) suggest.”
- Prediction of the Madden–Julian oscillation with the POAMA dynamical prediction system (2011, methodology): “We also examine the dependence of the predictive skill on the initial phase of the MJO as given by its location in the RMM phase–space (e.g., Fig. 3). Although the MJO may propagate around the entire globe along the equator and events may start or end in any phase (see also Matthews 2008 ), there a”
- MJO Initiation in the Real-Time Multivariate MJO Index (2013, methodology): “Unauthenticated | Downloaded 12/13/22 05:59 PM UTC Traditionally, the MJO itself has been identified based on some measure of cloudiness or convective heating and, less frequently, on the upper tropospheric divergent circulation.”
- Structure and Properties of Madden–Julian Oscillations Deduced from DYNAMO Sounding Arrays (2013, background): “…RAMA buoy at 1.5 8 S, 90 8 E, time series of 3-hourly average TRMM 3B42 rainfall (mmh 2 1 ) within a 1 8 radius of same buoy, hourly wind speed (ms 2 1 ) atsamebuoy,and timeseriesof dailyaveragedsealevelpressure(hPa)atRAMAbuoy at 0 8 , 80.5 8 E. November, followed by cooling into early December.”
- Atmosphere‐ocean coupled processes in the Madden‐Julian oscillation (2015, background): “…a prior MJO), development of MJO convection follows the suppressed phase; “primary” events (those not preceded by another MJO) appear to initiate locally [Matthews, 2008], although they, too, may be preceded by atmospheric wind anomalies [Straub, 2013; Ling et al., 2013; Haertel et al., 2015].”
- Prediction and monitoring of monsoon intraseasonal oscillations over Indian monsoon region in an ensemble prediction system using CFSv2 (2013, background): “The large event-to-event variability of the tropical ISO (Matthews 2008) imposes real challenge to the extended range forecast of MISO.”
- Predictability of the Madden–Julian Oscillation in the Intraseasonal Variability Hindcast Experiment (ISVHE)* (2014, background): “…the eight models, including the dependence of predictability on the amplitude and phase of MJO at hindcast initiation, are presented in section 4a. Analysis of whether the primary and secondary MJO events (Matthews 2008; Straub 2013) have different predictability is also explored in this section.”
- 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…”
- Three-Dimensional Structure and Evolution of the MJO and Its Relation to the Mean Flow (2014, background): “10c strong flanking Rossby waves are also seen over the Indian Ocean sector just to the south of the climatologicalmean jet streams, causing the jet stream to vary in strength, as noted by Yang and Webster (1990), Matthews and Kiladis (1999), andMoore et al. (2010).”