References
Hattori, M., et al. (2011).
Journal of the Meteorological Society of Japan 89A: 27-47.
62 CENS events in 1999-2009 DJFM: CENS can be categorized into 3 different types after focusing convective activities over Java island.
11 events of CS type: cold surge extending over the equator strong convection localized over Java Sea
20 events of MJO type: related to MJO without cold surge broad moderate convection over Maritime Continent.
16 events of CS-MJO type: related to MJO with cold surge strong broad convection centralized Java island.
Wu, P., et al. (2013).
Sola 9(0): 79-83.
2013/1/15-18 Jakarta torrential rain (193mm/4days) associated with MJO and cold surge is investigated by using BMKG radars.
Mori, S., et al. (2018).
Progress in Earth and Planetary Science 5(1).
Diurnal rainfall meridional march (DRMM) is investigated.
During MJO suppressed phase, diurnal convection basically migrates northward at 5 m/s from the mountainous area to the coastal area in association with land-sea/mountain-valley breeze circulation.
However during the phase of intensified CENS, diurnal convection migrating northward in nighttime returns back southward at 2 m/s in daytime.
Hattori, M., et al. (2011).
Journal of the Meteorological Society of Japan 89A: 27-47.
Hattori, M., et al. (2017).
Sola 13(0): 19-24.
Koseki, S., et al. (2013).
Quarterly Journal of the Royal Meteorological Society 139(675): 1566-1582.
Mori, S., et al. (2018).
Progress in Earth and Planetary Science 5(1).
Wu, P., et al. (2013).
Sola 9(0): 79-83.