MADDEN JULIAN OSCILLATION - GEOGRAPHY

News: Cyclone may affect course of monsoon

 

What is in the news?

       Recently, Cyclone Biparjoy in the Arabian Sea intensified into a very severe cyclone.

 

Key details of the Cyclone:

       It is expected to move northwards and turn towards Oman in the coming days.

       While this will help the monsoon onset in Kerala.

       An exceptionally warm Arabian Sea, a weak monsoon onset, and favorable Madden Julian Oscillation (MJO) conditions in the Indian Ocean are favoring this cyclone.

Madden Julian Oscillation Condition:

       The Madden-Julian Oscillation (MJO) is the largest element of intraseasonal variability in tropical weather.

       It is characterized as an eastward movement of enhanced and suppressed tropical convection over a 30- to 60-day period, on average.

       In the enhanced phase, winds at the surface converge and air rises through the atmosphere.

       This rising motion allows air to cool and condense, bringing more rainfall.

       In the suppressed phase, winds converge higher up in the atmosphere, forcing air to sink and then diverge at the surface.

       The sinking air warms and dries, consequently suppressing rainfall.

       After a region of enhanced convection comes a region of suppressed convection.

       Monsoon break in the August first week is caused by the Madden Julian Oscillation.

       The MJO phases

       Phase 1 – Enhanced convection (rainfall) develops over the western Indian Ocean.

       Phase 2 and 3 – Enhanced convection (rainfall) moves slowly eastwards over Africa, the Indian Ocean and parts of the Indian subcontinent. 

       Phase 4 and 5 – Enhanced convection (rainfall) has reached the Maritime Continent (Indonesia and West Pacific)

       Phase 6, 7 and 8 – Enhanced rainfall moves further eastward over the western Pacific, eventually dying out in the central Pacific.