Effect of Parameter Variation in the BMJ Scheme on the Simulation of MJO Propagation and Structure  

作　　者：Xiaoyu ZHU Zhong ZHONG Yimin ZHU Yunying LI Yijia HU Yao HA 

机构地区：[1]College of Meteorology and Oceanography,National University of Defense Technology,Changsha 410073,China [2]Key Laboratory for Virtual Geographic Environment,School of Geography Science,Nanjing Normal University,Nanjing 210023,China [3]Jiangsu Collaborative Innovation Center for Climate Change,School of Atmospheric Sciences,Nanjing University,Nanjing 210023,China

出　　处：《Advances in Atmospheric Sciences》2025年第2期397-409,共13页大气科学进展(英文版)

基　　金：supported by the National Natural Science Foundation of China(Grant Nos.41975090,U2242201,42075077);the Natural Science Foundation of Hunan Province,China(2022JJ20043);the Science and Technology Innovation Program of Hunan Province,China(2022RC1239)。

摘　　要：In this study,the Betts-Miller-Janjic(BMJ)convective adjustment scheme in the Weather Research and Forecasting(WRF)model version 4.0 was used to investigate the effect of itsα-parameter,which influences the first-guess potential temperature reference profile on the Madden-Julian oscillation(MJO)propagation and structure.This study diagnosed the MJO active phase composites of the MJO-filtered outgoing longwave radiation(OLR)during the December-to-February(DJF)period of 2006-2016 over the Indian Ocean(IO),Maritime Continent(MC),and western Pacific(WP).The results show that the MJO-filtered OLR intensity,propagation pattern,and MJO classification(standing,jumping,and propagating clusters)are sensitive to theα-value,but the phase speeds of propagating MJOs are not.Overall,with an increasingα-value,the simulated MJO-filtered OLR intensity increases,and the simulated propagation pattern is improved.Results also show that the intensity and propagation pattern of an eastward-propagating MJO are associated with MJO circulation structures and thermodynamic structures.Asαincreases,the front Walker cell and the low-level easterly anomaly are enhanced,which premoistens the lower troposphere and triggers more active shallow and congestus clouds.The enhanced shallow and congestus convection preconditions the lower to middle troposphere,accelerating the transition from congestus to deep convection,thereby facilitating eastward propagation of the MJO.Therefore,the simulated MJO tends to transfer from standing to eastward propagating asαincreases.In summary,increasing theα-value is a possible way to improve the simulation of the structure and propagation of the MJO.

关 键 词：MJO WRF model BMJ scheme low-level easterly anomaly 

分 类 号：P43[天文地球—大气科学及气象学]