Why does the MJO detour the Maritime Continent during austral summer?

• Published in: Geophysical research letters Vol. 44; no. 5; pp. 2579 - 2587
• Main Authors: Kim, Daehyun, Kim, Hyerim, Lee, Myong‐In
• Format: Journal Article
• Language: English
• Published: Washington John Wiley & Sons, Inc 16.03.2017
• Subjects: Advection; Anomalies; Area; Banks (topography); Continents; Convective activity; Cyclones; detour; eastward propagation; Energy budget; Energy budgets; Interactions; Madden-Julian oscillation; Maritime Continent; Meridional wind; Meteorology; MJO; Moist static energy; Moisture; moisture advection; Moisture gradient; Monsoons; Propagation; Recharging; Regional analysis; Slope; Summer; Topography; Topography (geology); Wind; Winds; Australia
• ISSN: 0094-8276; 1944-8007
• DOI: 10.1002/2017GL072643

Eastward propagation of the Madden‐Julian Oscillation (MJO) detours the Maritime Continent (MC) region southward during austral summer, exhibiting enhanced convective activity preferentially in the southern part of the MC area with much weaker anomalies in the central MC area. Column‐integrated moist static energy budget of the MJO is analyzed to understand the processes responsible for the MJO detouring. Results show that zonal and meridional moisture advection is the essential process to the MJO detouring, causing the difference between the southern and central MC regions in the moisture recharge before and during the MJO onset. Further analysis reveals that moisture advection by MJO perturbation winds acting upon the background moisture gradient has the dominant contribution to the regional contrast between the central and southern MC areas. The zonal moisture advection is greater in the southern MC region because the zonal gradient of the background moisture field is much steeper in the southern MC area than in the central MC area. The onset of the Australian monsoon in austral summer contributes to the establishment of the sharp zonal moisture gradient in the southern MC region. The meridional moisture advection is weaker in the central MC area because meridional wind anomalies associated with the MJO vary regionally, presumably through interactions with the topography and land‐sea contrast. Key Points Column‐integrated moist static energy budget of the MJO is analyzed to understand the processes responsible for the MJO detouring Horizontal moisture advection is the essential process to the detouring, causing the difference between the southern and central MC regions Zonal moisture advection by MJO winds acting upon the background moisture gradient has a large regional contrast between the two regions