How does this work? As the MJO moves through the Pacific, it strengthens convection near the dateline, further weakening the Walker Circulation. One ramification of this is anomalous eq. westerlies (I.E. WWBs), which reinforce the oceanic component of ENSO through downwelling. pic.twitter.com/XeDbyFkK5p

— Deelan Jariwala (@WxTca) November 24, 2023