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contributor authorKim, Daehyun
contributor authorKug, Jong-Seong
contributor authorSobel, Adam H.
date accessioned2017-06-09T17:08:17Z
date available2017-06-09T17:08:17Z
date copyright2014/01/01
date issued2013
identifier issn0894-8755
identifier otherams-79957.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4222794
description abstractasinwide convective anomalies over the Indian Ocean (IO) associated with the Madden?Julian oscillation (MJO) sometimes propagate eastward and reach the west Pacific (WP), but sometimes do not. Long-term observations and reanalysis products are used to investigate the difference between the propagating and nonpropagating MJO events. IO convection onset events associated with the MJO are grouped into three categories based on the strengths of the simultaneous dry anomalies over the eastern Maritime Continent and WP. The IO convection anomaly preferentially makes eastward propagation and reaches the WP when the dry anomaly is stronger.Analysis of the column-integrated moist static energy (MSE) budget shows that horizontal advection moistens the atmosphere to the east of the positive MSE anomaly associated with the active convection over the IO and is of sufficient magnitude to explain the eastward propagation of the positive MSE anomaly. Interpretation is complicated, however, by lack of closure in the MSE budget. A residual term, of smaller but comparable magnitude to the horizontal advection, also moistens the column to the east of the positive MSE anomaly. Nonetheless, the authors decompose the horizontal advection term into contributions from different scales and find that a dominant contribution is from free-tropospheric meridional advection by the intraseasonal time scale wind anomalies. The positive meridional advection in between the convective and dry anomalies is induced by the anomalous poleward flow, which is interpreted as part of the Rossby wave response to the dry anomaly. The poleward flow advects the climatological MSE, which peaks at the equator, and moistens to the east of IO convective anomaly.
publisherAmerican Meteorological Society
titlePropagating versus Nonpropagating Madden–Julian Oscillation Events
typeJournal Paper
journal volume27
journal issue1
journal titleJournal of Climate
identifier doi10.1175/JCLI-D-13-00084.1
journal fristpage111
journal lastpage125
treeJournal of Climate:;2013:;volume( 027 ):;issue: 001
contenttypeFulltext


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