Stratospheric Influences on the MJO-Induced Rossby Wave Train: Effects on Intraseasonal Climate
AffiliationUniv Arizona, Lunar & Planetary Lab
MetadataShow full item record
PublisherAMER METEOROLOGICAL SOC
CitationHood, L. L., Redman, M. A., Johnson, W. L., & Galarneau Jr, T. J. (2020). Stratospheric Influences on the MJO-Induced Rossby Wave Train: Effects on Intraseasonal Climate. Journal of Climate, 33(1), 365-389.
JournalJOURNAL OF CLIMATE
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AbstractThe tropical Madden–Julian oscillation (MJO) excites a northward propagating Rossby wave train that largely determines the extratropical surface weather consequences of the MJO. Previous work has demonstrated a significant influence of the tropospheric El Niño–Southern Oscillation (ENSO) on the characteristics of this wave train. Here, composite analyses of ERA-Interim sea level pressure (SLP) and surface air temperature (SAT) data during the extended northern winter season are performed to investigate the additional role of stratospheric forcings [the quasi-biennial oscillation (QBO) and the 11-yr solar cycle] in modifying the wave train and its consequences. MJO phase composites of 20–100-day filtered data for the two QBO phases show that, similar to the cool phase of ENSO, the easterly phase of the QBO (QBOE) produces a stronger wave train and associated modulation of SLP and SAT anomalies. In particular, during MJO phases 5–7, positive SLP and negative SAT anomalies in the North Atlantic/Eurasian sector are enhanced during QBOE relative to the westerly phase of the QBO (QBOW). The opposite occurs during the earliest MJO phases. SAT anomalies over eastern North America are also more strongly modulated during QBOE. Although less certain because of the short data record, there is some evidence that the minimum phase of the solar cycle (SMIN) produces a similar increased modulation of SLP and SAT anomalies. The strongest modulations of SLP and SAT anomalies are produced when two or more of the forcings are superposed (e.g., QBOE/cool ENSO, SMIN/QBOE, etc.).
Note6 month embargo; published online: 12 December 2019
VersionFinal published version
SponsorsClimate and Large-Scale Dynamics program of the National Science Foundation (NSF) - Directorate for Geosciences (GEO)