[University of St. Andrews] New research from the University of St Andrews has uncovered a thus unknown process which may have helped drive the Earth in to past ice ages.
![Meridional overturning streamfunction (Ψ). Meridional sections of zonally–integrated streamfunction (Sverdrups, 1 Sv ≡ 10 6 m 3 s−1 ) in the (a) IG_Ctrl, (b) Glac_Ref, (c) IG_N50, and (d) IG_N100 simulations. Positive (red) values denote clockwise overturning, while negative (blue) values denote counterclockwise overturning. The apparent diapycnal transport at ~60°S in (a) IG_Ctrl and (c) IG_N50 may be related to the effect of standing meanders [see Jansen (2017)] but does not impinge upon our results. -- Journal of Climate](https://i0.wp.com/astrobiology.com/wp-content/uploads/2026/10/New-discovery.png?resize=1200%2C720&ssl=1)
[University of St. Andrews] New research from the University of St Andrews has uncovered a thus unknown process which may have helped drive the Earth in to past ice ages.