Doubling of SSW occurrence and significant warmer & weaker polar vortex due to stronger MJO as expected in a warmer climate.
Background zonal asymmetry allows MJO to either enhance or suppress the SSWs
MJO-like forcings at different longitudinal locations drive the SSWs to different fates: interaction with the mid-latitude jet zonal asymmetry. read more…
Tropical and Extratropical General Circulation with a Meridional Reversed Temperature Gradient as Expected in a High Obliquity Planet. read more…
Why are high obliquity aquaplanets always warmer than low obliquity equivalents? read more…
Wanying Kang 