Stratospheric Influences on the MJO-Induced Rossby Wave Train: Effects on Intraseasonal Climate

• Published in: Journal of Climate
• Main Authors: Hood, Lon L., Redman, Malori A., Johnson, Wes L., Galarneau, Thomas J.
• Other Authors: Univ Arizona, Lunar & Planetary Lab
• Format: Article in Journal/Newspaper
• Language: English
• Published: AMER METEOROLOGICAL SOC 2019
• Subjects: ENSO; Madden-Julian oscillation; Quasibiennial oscillation; Rossby waves; Stability; Stratospheric circulation; North Atlantic
• Online Access: http://hdl.handle.net/10150/636703; https://doi.org/10.1175/jcli-d-18-0811.1

The 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.). Climate and Large-Scale Dynamics program of the National Science Foundation (NSF) - Directorate for Geosciences (GEO) [1643160] 6 month embargo; published online: 12 December 2019 This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at [e-mail].